173 results on '"Poli, Paul"'
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2. Typology and Mapping of Plant Landscape of Biguglia Pond: Application to Planning and Conservation Management
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Delbosc, Pauline, Bioret, Frédéric, Etourneau, Sabrina, Panaïotis, Christophe, Piazza, C., Poli, Paul, Pedrotti, Franco, Series Editor, Bartha, S., Editorial Board Member, Bioret, F., Editorial Board Member, Box, E. O., Editorial Board Member, Čarni, A., Editorial Board Member, Fujiwara, K., Editorial Board Member, Gafta, D., Editorial Board Member, Loidi, J., Editorial Board Member, Mucina, L., Editorial Board Member, Pignatti, S., Editorial Board Member, Pott, R., Editorial Board Member, Sánchez Mata, D., Editorial Board Member, Velázquez, A., Editorial Board Member, Venanzoni, R., Editorial Board Member, Delbosc, Pauline, editor, Bioret, Frédéric, editor, and Panaïotis, Christophe, editor
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- 2020
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3. Balloon drift estimation and improved position estimates for radiosondes
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Voggenberger, Ulrich, primary, Haimberger, Leopold, additional, Ambrogi, Federico, additional, and Poli, Paul, additional
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- 2023
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4. OBSERVATIONS FOR REANALYSES
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Brönnimann, Stefan, Allan, Rob, Atkinson, Christopher, Buizza, Roberto, Bulygina, Olga, Dahlgren, Per, Dee, Dick, Dunn, Robert, Gomes, Pedro, John, Viju O., Jourdain, Sylvie, Haimberger, Leopold, Hersbach, Hans, Kennedy, John, Poli, Paul, Pulliainen, Jouni, Rayner, Nick, Saunders, Roger, Schulz, Jörg, Sterin, Alexander, Stickler, Alexander, Titchner, Holly, Valente, Maria Antonia, Ventura, Clara, and Wilkinson, Clive
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- 2018
5. ADVANCING GLOBAL AND REGIONAL REANALYSES
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Buizza, Roberto, Poli, Paul, Rixen, Michel, Alonso-Balmaseda, Magdalena, Bosilovich, Michael G., Brönnimann, Stefan, Compo, Gilbert P., Dee, Dick P., Desiato, Franco, Doutriaux-Boucher, Marie, Fujiwara, Masatomo, Kaiser-Weiss, Andrea K., Kobayashi, Shinya, Liu, Zhiquan, Masina, Simona, Mathieu, Pierre-Philippe, Rayner, Nick, Richter, Carolin, Seneviratne, Sonia I., Simmons, Adrian J., Thépaut, Jean-Noel, Auger, Jeffrey D., Bechtold, Michel, Berntell, Ellen, Dong, Bo, Kozubek, Michal, Sharif, Khaled, Thomas, Christopher, Schimanke, Semjon, Storto, Andrea, Tuma, Matthias, Välisuo, Ilona, and Vaselali, Alireza
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- 2018
6. Assessing reanalysis quality with early sounders Nimbus-4 IRIS (1970) and Nimbus-6 HIRS (1975)
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Poli, Paul and Brunel, Pascal
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- 2018
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7. RECENT ADVANCES IN SATELLITE DATA RESCUE
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Poli, Paul, Dee, Dick P., Saunders, Roger, John, Viju O., Rayer, Peter, Schulz, Jörg, Holmlund, Kenneth, Coppens, Dorothee, Klaes, Dieter, Johnson, James E., Esfandiari, Asghar E., Gerasimov, Irina V., Zamkoff, Emily B., Al-Jazrawi, Atheer F., Santek, David, Albani, Mirko, Brunel, Pascal, Fennig, Karsten, Schröder, Marc, Kobayashi, Shinya, Oertel, Dieter, Döhler, Wolfgang, Spänkuch, Dietrich, and Bojinski, Stephan
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- 2017
8. SUPPLEMENT : RECENT ADVANCES IN SATELLITE DATA RESCUE
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Poli, Paul, Dee, Dick P., Saunders, Roger, John, Viju O., Rayer, Peter, Schulz, Jörg, Holmlund, Kenneth, Coppens, Dorothee, Klaes, Dieter, Johnson, James E., Esfandiari, Asghar E., Gerasimov, Irina V., Zamkoff, Emily B., Al-Jazrawi, Atheer F., Santek, David, Albani, Mirko, Brunel, Pascal, Fennig, Karsten, Schröder, Marc, Kobayashi, Shinya, Oertel, Dieter, Döhler, Wolfgang, Spänkuch, Dietrich, and Bojinski, Stephan
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- 2017
9. Characterisation of Special Sensor Microwave Water Vapor Profiler (SSM/T-2) radiances using radiative transfer simulations from global atmospheric reanalyses
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Kobayashi, Shinya, Poli, Paul, and John, Viju O.
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- 2017
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10. Balloon drift estimation and improved position estimates for radiosondes.
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Voggenberger, Ulrich, Haimberger, Leopold, Ambrogi, Federico, and Poli, Paul
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GLOBAL Positioning System ,RADIOSONDES ,KALMAN filtering ,SURFACE of the earth - Abstract
When comparing model output with historical radiosonde observations, it is usually assumed that the radiosonde has risen exactly above its starting point and has not been displaced by the wind. This has changed only relatively recently with the availability of Global Navigation Satellite System (GNSS) receivers aboard the radiosondes in the late-1990s, but even then the balloon trajectory data were often not transmitted, although this information was the basis for estimating the wind in the first place. Depending on the conditions and time of year, radiosondes can sometimes drift a few hundred kilometres, particularly in the mid-latitudes during the winter months. The position errors can lead to non-negligible representation errors when the corresponding observations are assimilated. This paper presents a methodology to compute changes in the balloon position during its vertical ascent, using only limited information, such as the vertical profile of wind contained in the historical observation reports. The sensitivity of the method to various parameters is investigated, such as the vertical resolution of the input data, the assumption about vertical ascent speed of the balloon, and the departure of the surface of the Earth from a sphere. The paper considers modern GNSS sonde data reports for validation, for which the full trajectory of the balloon is available, alongside the estimated wind. Evaluation is also conducted by comparison with ERA5 and by conducting low-resolution data assimilation experiments. Overall, the results indicate that the trajectory of the radiosonde can be accurately reconstructed from original data of varying vertical resolution and that the more accurate balloon position reduces representation errors, and, in some cases, also systematic errors. [ABSTRACT FROM AUTHOR]
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- 2023
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11. List of Contributors
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Achterberg, Eric P., primary, Allen, Simon, additional, Alves, José C., additional, Aragon, David, additional, Au, Douglas, additional, Barnes, Christopher R., additional, Barus, Carole, additional, Beaton, Alex, additional, Bell, Ryan J., additional, Blouch, Pierre, additional, Brault, Patrice, additional, Carvalho, Filipa, additional, Cervantes, Pablo, additional, Chen Legrand, D., additional, Colas, Florent, additional, Cowles, Timothy, additional, Cruz, Nuno A., additional, David, Arnaud, additional, Fernandez, Joaquin del Rio, additional, Delauney, Laurent, additional, Delory, Eric, additional, Dewitte, Boris, additional, Ferreira, Bruno M., additional, Fischer, Albert, additional, Garçon, Veronique, additional, Glenn, Scott, additional, Harcourt, Robert, additional, Heupel, Michelle R., additional, Jirka, Simon, additional, Jońca, Justyna, additional, Jones, Clayton, additional, Jugeau, Benoit, additional, Kibelka, Gottfried P.G., additional, Kim Juniper, S., additional, Kohut, Josh, additional, Laspidou, Chrysi, additional, Leadbetter, Adam, additional, Leblond, Emilie, additional, Lédée, E.J.I., additional, Mahfuz, Hassan, additional, Manes, Carmem-Lara, additional, Martinez, Enoc, additional, Martinez, Sergio, additional, Matos, Aníbal C., additional, McDonnell, Janice, additional, McLean, Scott, additional, Memè, Simone, additional, Toma, Daniel Mihai, additional, Miles, Travis, additional, Sabet, Seyed Morteza, additional, Mowlem, Matthew, additional, Muñoz Parra, P., additional, O’Reilly, Tom, additional, Ove Möller, Klas, additional, Pearlman, Jay, additional, Petersen, Wilhelm, additional, Pirenne, Benoît, additional, Poli, Paul, additional, Precheur, Hervé, additional, Quemener, Loïc, additional, Ralston, Emily, additional, Ramos, Marcel, additional, Reitz, Anja, additional, Rieke, Matthes, additional, Roarty, Hugh, additional, Romanytsia, Ivan, additional, Round, Adrian, additional, Ruiz, Pablo, additional, Saba, Grace, additional, Schaap, Allison, additional, Schofield, Oscar, additional, Seroka, Greg, additional, Stasch, Christoph, additional, Striebig, Nicolas, additional, Timothy Short, R., additional, Toler, Strawn K., additional, Udyawer, Vinay, additional, Valladares, Maria, additional, Visbeck, Martin, additional, Walsh, Ian, additional, Wild-Allen, Karen, additional, Woerther, Patrice, additional, Woillez, Mathieu, additional, Wollschläger, Jochen, additional, Yi, Xu, additional, and Hunsucker, Kelli Zargiel, additional
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- 2019
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12. OBSERVATIONS FOR REANALYSES: Reanalysis efforts depend on observations and the corresponding work feeds into public Repositories, ideally occurring one cycle ahead of reanalysis generation
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Bronnimann, Stefan, Allan, Rob, Atkinson, Christopher, Buizza, Roberto, Bulygina, Olga, Dahlgren, Per, Dee, Dick, Dunn, Robert, Gomes, Pedro, John, Viju O., Jourdain, Sylvie, Haimberger, Leopold, Hersbach, Hans, Kennedy, John, Poli, Paul, Pulliainen, Jouni, Rayner, Nick, Saunders, Roger, Schulz, Jorg, Sterin, Alexander, Stickler, Alexander, Titchner, Holly, Valente, Maria Antonia, Ventura, Clara, and Wilkinson, Clive
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Meteorological satellites -- Information management ,Meteorological research -- Information management ,Oceanographic research -- Information management ,Company systems management ,Business ,Earth sciences - Abstract
Global dynamical reanalyses of the atmosphere and ocean fundamentally rely on observations, not just for the assimilation (i.e., for the definition of the state of the Earth system components) but [...]
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- 2018
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13. Development of a Quasi-Global Fundamental Climate Data Record for Observations from Geostationary Satellites
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Roebeling, Rob, primary, John, Viju, additional, Schulz, Joerg, additional, Onderwaater, Jaap, additional, Sus, Oliver, additional, Knapp, Ken R., additional, Heidinger, Andrew, additional, Tabata, Tasuku, additional, Okuyama, Arata, additional, Ruethrich, Frank, additional, Poli, Paul, additional, Grant, Mike, additional, Tervo, Roope, additional, and Hanschmann, Timo, additional
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- 2023
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14. Radiance Simulations in Support of Climate Services
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Poli, Paul, primary, Roebeling, Rob, additional, John, Viju Oommen, additional, Doutriaux-Boucher, Marie, additional, Schulz, Joerg, additional, Lattanzio, Alessio, additional, Petraityte, Kristina, additional, Grant, Mike, additional, Hanschmann, Timo, additional, Onderwaater, Jacobus, additional, Sus, Oliver, additional, Huckle, Roger, additional, Coppens, Dorothee, additional, Théodore, Bertrand, additional, August, Thomas, additional, Simmons, Adrian John, additional, Bell, William, additional, Mittaz, Jonathan, additional, Hall, Thomas, additional, Vidot, Jerome, additional, Brunel, Pascal, additional, Johnson, James E., additional, Zamkoff, Emily B., additional, Al-Jazrawi, Atheer F., additional, Esfandiari, Asghar E., additional, Gerasimov, Irina V., additional, and Kobayashi, Shinya, additional
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- 2023
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15. ERA-20C : An Atmospheric Reanalysis of the Twentieth Century
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Poli, Paul, Hersbach, Hans, Dee, Dick P., Berrisford, Paul, Simmons, Adrian J., Vitart, Frédéric, Laloyaux, Patrick, Tan, David G. H., Peubey, Carole, Thépaut, Jean-Noël, Trémolet, Yannick, Hólm, Elías V., Bonavita, Massimo, Isaksen, Lars, and Fisher, Michael
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- 2016
16. Comment on amt-2022-121
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Poli, Paul, primary
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- 2022
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17. Assimilation Experiments of One-dimensional Variational Analyses with GPS/MET Refractivity
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Poli, Paul, Joiner, Joanna, Reigber, Christoph, editor, Lühr, Hermann, editor, and Schwintzer, Peter, editor
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- 2003
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18. DBCP Drifting Buoys GDAC data management report 2021
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Carval, Thierry, Ma, Zhimin, Guillerm, Christophe, Gaboury, Isabelle, Emzivat, Gilbert, and Poli, Paul
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This report covers the activity of Drifting Data Buoys Global Data Assembly Centre (DDB GDAC) published for Data Buoy Cooperation Panel (DBCP) Thirty Seventh Session.
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- 2021
19. Assimilation of satellite observations of the atmosphere
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Poli, Paul
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- 2010
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20. Le voilier OceanoScientific Explorer Boogaloo : Une campagne péri-antarctique en 2017
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Reverdin, Gilles, primary, Metzl, Nicolas, additional, Reynaud, Thierry, additional, Poli, Paul, additional, and Griboval, Yvan, additional
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- 2020
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21. Report of the 4th World Climate Research Programme International Conference on Reanalyses
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Bosilovich, Michael G, Rixen, Michel, van Oevelen, Peter, Asrar, Ghassem, Compo, Gilbert, Onogi, Kazutoshi, Simmons, Adrian, Trenberth, Kevin, Behringer, Dave, Bhuiyan, Tanvir Hossain, Capps, Shannon, Chaudhuri, Ayan, Chen, Junye, Chen, Linling, Colasacco-Thumm, Nicole, Escobar, Maria Gabriela, Ferguson, Craig R, Ishibashi, Toshiyuki, Liberato, Margarida L. R, Meng, Jesse, Molod, Andrea, Poli, Paul, Roundy, Joshua, Willett, Kate, and Wollen, Jack
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Meteorology And Climatology - Abstract
The 4th WCRP International Conference on Reanalyses provided an opportunity for the international community to review and discuss the observational and modelling research, as well as process studies and uncertainties associated with reanalysis of the Earth System and its components. Characterizing the uncertainty and quality of reanalyses is a task that reaches far beyond the international community of producers, and into the interdisciplinary research community, especially those using reanalysis products in their research and applications. Reanalyses have progressed greatly even in the last 5 years, and newer ideas, projects and data are coming forward. While reanalysis has typically been carried out for the individual domains of atmosphere, ocean and land, it is now moving towards coupling using Earth system models. Observations are being reprocessed and they are providing improved quality for use in reanalysis. New applications are being investigated, and the need for climate reanalyses is as strong as ever. At the heart of it all, new investigators are exploring the possibilities for reanalysis, and developing new ideas in research and applications. Given the many centres creating reanalyses products (e.g. ocean, land and cryosphere research centres as well as NWP and atmospheric centers), and the development of new ideas (e.g. families of reanalyses), the total number of reanalyses is increasing greatly, with new and innovative diagnostics and output data. The need for reanalysis data is growing steadily, and likewise, the need for open discussion and comment on the data. The 4th Conference was convened to provide a forum for constructive discussion on the objectives, strengths and weaknesses of reanalyses, indicating potential development paths for the future.
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- 2012
22. The Copernicus surface velocity platform drifter with barometer and reference sensor for temperature (SVP-BRST):\ud genesis, design, and initial results
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Poli, Paul, Lucas, Marc, O'Carroll, Anne, Le Menn, Marc, David, Arnaud, Corlett, Gary K., Blouch, Pierre, Meldrum, David, Merchant, Christopher J., Belbeoch, Mathieu, and Herklotz, Kai
- Abstract
To support calibration and validation of satel- lite sea surface temperature (SST) retrievals, over 60 high- resolution SST (HRSST) drifting buoys were deployed at sea between 2012 and 2017. Their data record is reviewed here. It is confirmed that sea state and immersion depth play an important role in understanding the data collected by such buoys and that the SST sensors need adequate insu- lation. In addition, calibration verification of three recovered drifters suggests that the sensor drift is low, albeit negative at around −0.01 K year−1. However, the statistical significance of these results is limited, and the calibration procedure could not be exactly reproduced, introducing additional uncertain- ties into this drift assessment. Based on lessons learnt from these initial buoys, a new sensor package for the Surface Velocity Platform with Barometer (SVP-B) was designed to serve calibration of SST retrievals by European Union’s Copernicus satellites. The novel sensor package includes an HRSST sensor calibrated by a metrology laboratory. The sensor includes a pressure probe to monitor immersion depth in calm water and acquires SST data at 1 Hz over a 5 min in-\ud terval every hour. This enables the derivation of mean SST as well as several percentiles of the SST distribution. The HRSST sensor is calibrated with an uncertainty better than 0.01 K. Analysis of the data collected by two prototypes de- ployed in the Mediterranean Sea shows that the buoys are able to capture small-scale SST variations. These variations are found to be smaller when the sea state is well mixed and when the buoys are located within eddy cores. This affects the drifter SST data representativeness, which is an aspect of importance for optimal use of these data.
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- 2019
23. Refined AtlantOS Requirements Report
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Ott, Michael, Fischer, Albert, Buch, Erik, Charria, Guillaume, Lherminier, Pascale, Claustre, Herve, Le Traon, Pierre-Yves, Tanhua, Toste, Edwards, Martin, Wölfl, Anne-Cathrin, Devey, Colin W., Pouliquen, Sylvie, Schauer, Ursula, Karstensen, Johannes, Araujo, Moacyr, Poli, Paul, and Afonso, Pedro
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13. Climate action ,14. Life underwater - Abstract
Refined description from AtlantOS work of the societal imperatives for sustained Atlantic Ocean observations, the phenomena to observe, EOVs, and contributing observing networks.
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- 2019
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24. Ship-Based Contributions to Global Ocean, Weather, and Climate Observing Systems
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Smith, Shawn R., Alory, Gaël, Andersson, Axel, Asher, William, Baker, Alex, Berry, David I., Drushka, Kyla, Figurskey, Darin, Freeman, Eric, Holthus, Paul, Jickells, Tim, Kleta, Henry, Kent, Elizabeth C., Kolodziejczyk, Nicolas, Kramp, Martin, Loh, Zoe, Poli, Paul, Schuster, Ute, Steventon, Emma, Swart, Sebastiaan, Tarasova, Oksana, Petit De La Villeon, Loic, Vinogradova-shiffer, Nadya, Smith, Shawn R., Alory, Gaël, Andersson, Axel, Asher, William, Baker, Alex, Berry, David I., Drushka, Kyla, Figurskey, Darin, Freeman, Eric, Holthus, Paul, Jickells, Tim, Kleta, Henry, Kent, Elizabeth C., Kolodziejczyk, Nicolas, Kramp, Martin, Loh, Zoe, Poli, Paul, Schuster, Ute, Steventon, Emma, Swart, Sebastiaan, Tarasova, Oksana, Petit De La Villeon, Loic, and Vinogradova-shiffer, Nadya
- Abstract
The role ships play in atmospheric, oceanic, and biogeochemical observations is described with a focus on measurements made near the ocean surface. Ships include merchant and research vessels; cruise liners and ferries; fishing vessels; coast guard, military, and other government-operated ships; yachts; and a growing fleet of automated surface vessels. The present capabilities of ships to measure essential climate/ocean variables and the requirements from a broad community to address operational, commercial, and scientific needs are described. The authors provide a vision to expand observations needed from ships to understand and forecast the exchanges across the ocean–atmosphere interface. The vision addresses (1) recruiting vessels to improve both spatial and temporal sampling, (2) conducting multivariate sampling on ships, (3) raising technology readiness levels of automated shipboard sensors and ship-to-shore data communications, (4) advancing quality evaluation of observations, and (5) developing a unified data management approach for observations and metadata that meet the needs of a diverse user community. Recommendations are made focusing on integrating private and autonomous vessels into the observing system, investing in sensor and communications technology development, developing an integrated data management structure that includes all types of ships, and moving toward a quality evaluation process that will result in a subset of ships being defined as mobile reference ships that will support climate studies. We envision a future where commercial, research, and privately owned vessels are making multivariate observations using a combination of automated and human-observed measurements. All data and metadata will be documented, tracked, evaluated, distributed, and archived to benefit users of marine data. This vision looks at ships as a holistic network, not a set of disparate commercial, research, and/or third-party activities working in isolation, to bri
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- 2019
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25. The Joint IOC (of UNESCO) and WMO Collaborative Effort for Met-Ocean Services
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Pinardi, Nadia, Stander, Johan, Legler, David M., O'Brien, Kevin, Boyer, Tim, Cuff, Tom, Bahurel, Pierre, Belbeoch, Mathieu, Belov, Sergey, Brunner, Shelby, Burger, Eugene, Carval, Thierry, Chang-seng, Denis, Charpentier, Etienne, Ciliberti, S., Coppini, Giovanni, Fischer, Albert, Freeman, Eric, Gallage, Champika, Garcia, Hernan, Gates, Lydia, Gong, Zhiqiang, Hermes, Juliet, Heslop, Emma, Grimes, Sarah, Hill, Katherine, Horsburgh, Kevin, Iona, Athanasia, Mancini, Sebastien, Moodie, Neal, Ouellet, Mathieu, Pissierssens, Peter, Poli, Paul, Proctor, Roger, Smith, Neville, Sun, Charles, Swail, Val, Turton, Jonathan, Xinyang, Yue, Pinardi, Nadia, Stander, Johan, Legler, David M., O'Brien, Kevin, Boyer, Tim, Cuff, Tom, Bahurel, Pierre, Belbeoch, Mathieu, Belov, Sergey, Brunner, Shelby, Burger, Eugene, Carval, Thierry, Chang-seng, Denis, Charpentier, Etienne, Ciliberti, S., Coppini, Giovanni, Fischer, Albert, Freeman, Eric, Gallage, Champika, Garcia, Hernan, Gates, Lydia, Gong, Zhiqiang, Hermes, Juliet, Heslop, Emma, Grimes, Sarah, Hill, Katherine, Horsburgh, Kevin, Iona, Athanasia, Mancini, Sebastien, Moodie, Neal, Ouellet, Mathieu, Pissierssens, Peter, Poli, Paul, Proctor, Roger, Smith, Neville, Sun, Charles, Swail, Val, Turton, Jonathan, and Xinyang, Yue
- Abstract
The WMO-IOC Joint Technical Commission for Oceanography and Marine Meteorology (JCOMM) has devised a coordination mechanism for the fit-for-purpose delivery of an end-to-end system, from ocean observations to met-ocean operational services. This paper offers a complete overview of the activities carried out by JCOMM and the status of the achievements up to 2018. The JCOMM stakeholders consist of the research and operational institutions of WMO members and the IOC member states, which mandated JCOMM to devise an international strategy to move toward the achievement of the United Nations Sustainable Development Goals. The three areas of activity are the Observation Program Area (OPA), the Data Management Program Area (DMPA) and the Services and Forecasting Services Program Area (SFSPA), and several expert teams have been established to contribute to the international coordination efforts. OPA is organized into observing networks connected by different observing technologies, DMPA organizes the overall near-real time and delayed mode data assembly, and the delivery methodology and architecture, and the SFSPA coordinates the met-ocean services resulting from the observations and data management. Future developments should enhance coordination in these three program areas by considering the inclusion of new and emergent observing technologies, the interoperability of met-ocean data assembly centers and the establishment of efficient research to operations protocols, in addition to better fit-for-purpose customized services in both the public and private sectors.
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- 2019
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26. Global in situ Observations of Essential Climate and Ocean Variables at the Air-Sea Interface
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Centurioni, Luca R., Turton, Jon, Lumpkin, Rick, Braasch, Lancelot, Brassington, Gary, Chao, Yi, Charpentier, Etienne, Chen, Zhaohui, Corlett, Gary, Dohan, Kathleen, Donlon, Craig, Gallage, Champika, Hormann, Verena, Ignatov, Alexander, Ingleby, Bruce, Jensen, Robert, Kelly-Gerreyn, Boris A., Koszalka, Inga M., Lin, Xiaopei, Lindstrom, Eric, Maximenko, Nikolai, Merchant, Christopher J., Minnett, Peter, O'Carroll, Anne, Paluszkiewicz, Theresa, Poli, Paul, Poulain, Pierre-Marie, Reverdin, Gilles, Sun, Xiujun, Swail, Val, Thurston, Sidney, Wu, Lixin, Yu, Lisan, Wang, Bin, Zhang, Dongxiao, Centurioni, Luca R., Turton, Jon, Lumpkin, Rick, Braasch, Lancelot, Brassington, Gary, Chao, Yi, Charpentier, Etienne, Chen, Zhaohui, Corlett, Gary, Dohan, Kathleen, Donlon, Craig, Gallage, Champika, Hormann, Verena, Ignatov, Alexander, Ingleby, Bruce, Jensen, Robert, Kelly-Gerreyn, Boris A., Koszalka, Inga M., Lin, Xiaopei, Lindstrom, Eric, Maximenko, Nikolai, Merchant, Christopher J., Minnett, Peter, O'Carroll, Anne, Paluszkiewicz, Theresa, Poli, Paul, Poulain, Pierre-Marie, Reverdin, Gilles, Sun, Xiujun, Swail, Val, Thurston, Sidney, Wu, Lixin, Yu, Lisan, Wang, Bin, and Zhang, Dongxiao
- Abstract
The air-sea interface is a key gateway in the Earth system. It is where the atmosphere sets the ocean in motion, climate/weather-relevant air-sea processes occur, and pollutants (i.e., plastic, anthropogenic carbon dioxide, radioactive/chemical waste) enter the sea. Hence, accurate estimates and forecasts of physical and biogeochemical processes at this interface are critical for sustainable blue economy planning, growth, and disaster mitigation. Such estimates and forecasts rely on accurate and integrated in situ and satellite surface observations. High-impact uses of ocean surface observations of essential ocean/climate variables (EOVs/ECVs) include (1) assimilation into/validation of weather, ocean, and climate forecast models to improve their skill, impact, and value; (2) ocean physics studies (i.e., heat, momentum, freshwater, and biogeochemical air-sea fluxes) to further our understanding and parameterization of air-sea processes; and (3) calibration and validation of satellite ocean products (i.e., currents, temperature, salinity, sea level, ocean color, wind, and waves). We review strengths and limitations, impacts, and sustainability of in situ ocean surface observations of several ECVs and EOVs. We draw a 10-year vision of the global ocean surface observing network for improved synergy and integration with other observing systems (e.g., satellites), for modeling/forecast efforts, and for a better ocean observing governance. The context is both the applications listed above and the guidelines of frameworks such as the Global Ocean Observing System (GOOS) and Global Climate Observing System (GCOS) (both co-sponsoredby the Intergovernmental Oceanographic Commission of UNESCO, IOC-UNESCO; the World Meteorological Organization, WMO; the United Nations Environment Programme, UNEP; and the International Science Council, ISC). Networks of multiparametric platforms, such as the global drifter array, offer opportunities for new and improved in situ observations. Adv
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- 2019
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27. The tropical Atlantic observing system
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Foltz, Gregory R., Brandt, Peter, Richter, Ingo, Rodriguez-fonseca, Belen, Hernandez, Fabrice, Dengler, Marcus, Rodrigues, Regina, Schmidt, Jörn Oliver, Yu, Lisan, Lefevre, Nathalie, Cotrim Da Cunha, Leticia, McPhaden, Michael J., Araujo, Moacyr, Karstensen, Johannes, Hahn, Johannes, Martín-Rey, Marta, Patricola, Christina, Poli, Paul, Zuidema, Paquita, Hummels, Rebecca, Perez, Renellys, Hatje, Vanessa, Luebbecke, Joke, Polo, Irene, Lumpkin, Rick, Bourlès, Bernard, Asuquo, Francis Emile, Lehodey, Patrick, Conchon, Anna, Chang, Ping, Dandin, Philippe, Schmid, Claudia, Sutton, Adrienne J., Giordani, Hervé, Xue, Yan, Illig, Serena, Losada, Teresa, Grodsky, Semyon A., Gasparin, Florent, Lee, Tong, Mohino, Elsa, Nobre, Paulo, Wanninkhof, Rik, Keenlyside, Noel S., Garcon, Veronique Cameille, Sanchez-Gomez, Emilia, Nnamchi, Hyacinth, Drevillon, Marie, Storto, Andrea, Remy, Elisabeth, Lazar, Alban, Speich, Sabrina, Goes, Marlos Pereira, Dorrington, Tarquin, Johns, William E., Moum, James N., Robinson, Carol, Perruche, Coralie, de Souza, Ronald Buss, Gaye, Amadou, Lopez-Parages, Jorge, Monerie, Paul-Arthur, Castellanos, Paola, Benson, Nsikak U., Hounkonnou, Mahouton Norbert, Trotte Duha, Janice, Laxenaire, Rémi, Reul, Nicolas, Foltz, Gregory R., Brandt, Peter, Richter, Ingo, Rodriguez-fonseca, Belen, Hernandez, Fabrice, Dengler, Marcus, Rodrigues, Regina, Schmidt, Jörn Oliver, Yu, Lisan, Lefevre, Nathalie, Cotrim Da Cunha, Leticia, McPhaden, Michael J., Araujo, Moacyr, Karstensen, Johannes, Hahn, Johannes, Martín-Rey, Marta, Patricola, Christina, Poli, Paul, Zuidema, Paquita, Hummels, Rebecca, Perez, Renellys, Hatje, Vanessa, Luebbecke, Joke, Polo, Irene, Lumpkin, Rick, Bourlès, Bernard, Asuquo, Francis Emile, Lehodey, Patrick, Conchon, Anna, Chang, Ping, Dandin, Philippe, Schmid, Claudia, Sutton, Adrienne J., Giordani, Hervé, Xue, Yan, Illig, Serena, Losada, Teresa, Grodsky, Semyon A., Gasparin, Florent, Lee, Tong, Mohino, Elsa, Nobre, Paulo, Wanninkhof, Rik, Keenlyside, Noel S., Garcon, Veronique Cameille, Sanchez-Gomez, Emilia, Nnamchi, Hyacinth, Drevillon, Marie, Storto, Andrea, Remy, Elisabeth, Lazar, Alban, Speich, Sabrina, Goes, Marlos Pereira, Dorrington, Tarquin, Johns, William E., Moum, James N., Robinson, Carol, Perruche, Coralie, de Souza, Ronald Buss, Gaye, Amadou, Lopez-Parages, Jorge, Monerie, Paul-Arthur, Castellanos, Paola, Benson, Nsikak U., Hounkonnou, Mahouton Norbert, Trotte Duha, Janice, Laxenaire, Rémi, and Reul, Nicolas
- Abstract
© The Author(s), 2019. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Foltz, G. R., Brandt, P., Richter, I., Rodriguez-Fonsecao, B., Hernandez, F., Dengler, M., Rodrigues, R. R., Schmidt, J. O., Yu, L., Lefevre, N., Da Cunha, L. C., Mcphaden, M. J., Araujo, M., Karstensen, J., Hahn, J., Martin-Rey, M., Patricola, C. M., Poli, P., Zuidema, P., Hummels, R., Perez, R. C., Hatje, V., Luebbecke, J. F., Palo, I., Lumpkin, R., Bourles, B., Asuquo, F. E., Lehodey, P., Conchon, A., Chang, P., Dandin, P., Schmid, C., Sutton, A., Giordani, H., Xue, Y., Illig, S., Losada, T., Grodsky, S. A., Gasparinss, F., Lees, T., Mohino, E., Nobre, P., Wanninkhof, R., Keenlyside, N., Garcon, V., Sanchez-Gomez, E., Nnamchi, H. C., Drevillon, M., Storto, A., Remy, E., Lazar, A., Speich, S., Goes, M., Dorrington, T., Johns, W. E., Moum, J. N., Robinson, C., Perruches, C., de Souza, R. B., Gaye, A. T., Lopez-Paragess, J., Monerie, P., Castellanos, P., Benson, N. U., Hounkonnou, M. N., Trotte Duha, J., Laxenairess, R., & Reul, N. The tropical Atlantic observing system. Frontiers in Marine Science, 6(206), (2019), doi:10.3389/fmars.2019.00206., he tropical Atlantic is home to multiple coupled climate variations covering a wide range of timescales and impacting societally relevant phenomena such as continental rainfall, Atlantic hurricane activity, oceanic biological productivity, and atmospheric circulation in the equatorial Pacific. The tropical Atlantic also connects the southern and northern branches of the Atlantic meridional overturning circulation and receives freshwater input from some of the world’s largest rivers. To address these diverse, unique, and interconnected research challenges, a rich network of ocean observations has developed, building on the backbone of the Prediction and Research Moored Array in the Tropical Atlantic (PIRATA). This network has evolved naturally over time and out of necessity in order to address the most important outstanding scientific questions and to improve predictions of tropical Atlantic severe weather and global climate variability and change. The tropical Atlantic observing system is motivated by goals to understand and better predict phenomena such as tropical Atlantic interannual to decadal variability and climate change; multidecadal variability and its links to the meridional overturning circulation; air-sea fluxes of CO2 and their implications for the fate of anthropogenic CO2; the Amazon River plume and its interactions with biogeochemistry, vertical mixing, and hurricanes; the highly productive eastern boundary and equatorial upwelling systems; and oceanic oxygen minimum zones, their impacts on biogeochemical cycles and marine ecosystems, and their feedbacks to climate. Past success of the tropical Atlantic observing system is the result of an international commitment to sustained observations and scientific cooperation, a willingness to evolve with changing research and monitoring needs, and a desire to share data openly with the scientific community and operational centers. The observing system must continue to evolve in order to meet an expanding set, MM-R received funding from the MORDICUS grant under contract ANR-13-SENV-0002-01 and the MSCA-IF-EF-ST FESTIVAL (H2020-EU project 797236). GF, MG, RLu, RP, RW, and CS were supported by NOAA/OAR through base funds to AOML and the Ocean Observing and Monitoring Division (OOMD; fund reference 100007298). This is NOAA/PMEL contribution #4918. PB, MDe, JH, RH, and JL are grateful for continuing support from the GEOMAR Helmholtz Centre for Ocean Research Kiel. German participation is further supported by different programs funded by the Deutsche Forschungsgemeinschaft, the Deutsche Bundesministerium für Bildung und Forschung (BMBF), and the European Union. The EU-PREFACE project funded by the EU FP7/2007–2013 programme (Grant No. 603521) contributed to results synthesized here. LCC was supported by the UERJ/Prociencia-2018 research grant. JOS received funding from the Cluster of Excellence Future Ocean (EXC80-DFG), the EU-PREFACE project (Grant No. 603521) and the BMBF-AWA project (Grant No. 01DG12073C).
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- 2019
28. Towards a traceable climate service: Assessment of quality and usability of essential climate variables
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Zeng, Yijian, Su, Zhongbo, Barmpadimos, Iakovos, Perrels, Adriaan, Poli, Paul, Boersma, K.F., Frey, Anna, Ma, Xiaogang, de Bruin, Karianne, Goosen, Hasse, John, Viju O., Roebeling, Rob, Schulz, Jörg, Timmermans, Wim, Zeng, Yijian, Su, Zhongbo, Barmpadimos, Iakovos, Perrels, Adriaan, Poli, Paul, Boersma, K.F., Frey, Anna, Ma, Xiaogang, de Bruin, Karianne, Goosen, Hasse, John, Viju O., Roebeling, Rob, Schulz, Jörg, and Timmermans, Wim
- Abstract
Climate services are becoming the backbone to translate climate knowledge, data & information into climate-informed decision-making at all levels, from public administrations to business operators. It is essential to assess the technical and scientific quality of the provided climate data and information products, including their value to users, to establish the relation of trust between providers of climate data and information and various downstream users. The climate data and information products (i.e., from satellite, in-situ and reanalysis) shall be fully traceable, adequately documented and uncertainty quantified and can provide sufficient guidance for users to address their specific needs and feedbacks. This paper discusses details on how to apply the quality assurance framework to deliver timely assessments of the quality and usability of Essential Climate Variable (ECV) products. It identifies an overarching structure for the quality assessment of single product ECVs (i.e., consists of only one single variable), multi-product ECVs (i.e., more than one single parameter), thematic products (i.e., water, energy and carbon cycles), as well as the usability assessment. To support a traceable climate service, other than rigorously evaluating the technical and scientific quality of ECV products, which represent the upstream of climate services, how the uncertainty propagates into the resulting benefit (utility) for the users of the climate service needs to be detailed.
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- 2019
29. Using Microwave and Infrared Radiances from Off-Nadir Pixels: Application of Radiative Transfer to Slanted Line-of-Sight and Comparisons with NASA EOS Aqua Data
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Poli, Paul and Joiner, Joanna
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Earth Resources And Remote Sensing - Abstract
The passive infrared and microwave nadir sounders such as (A)TOVS observe the atmosphere from a polar orbit by directing their scan pointed at the ground up to about 49 degrees from nadir. Except for the pixels located right on the satellite ground track, the radiance measurements collected by these instruments characterize hence atmospheric emission paths which are slanted with respect to the zenithal direction at the ground. At the outer swath edges, the deviations from nadir reach about 60 degrees in terms of Satellite Zenith Angle (SZA). The radiative transfer codes used in operational Numerical Weather Prediction applications make the appropriate corrections to account for the extra path induced by the non-zero SZA. However, no corrections are made to account for the fact that the atmospheric profiles along the slanted line-of-sight (LOS) are different from the vertical because of horizontal gradients in the atmosphere. Using NASA EOS Aqua satellite's orbits, zenith and azimuth angles, as well as three-dimensional fields of temperature, water vapor, and ozone produced by the NASA Global Modeling and Assimilation Office, we extracted slanted atmospheric profiles for actual soundings performed by the AIRS and AMSU-A instruments onboard EOS Aqua. We will present the results of our study comparing the calculated brightness temperatures along slanted LOS and vertical LOS with AIRS and AMSU-A observations.
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- 2005
30. The impact of ozone field horizontal inhomogeneities on nadir-viewing orbital backscatter UV measurements
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Mueller, Martin D, Poli, Paul, and Joiner, Joanna
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Meteorology And Climatology - Abstract
Radiative transfer calculations for nadir-viewing satellites normally assume the atmosphere to be horizontally homogeneous. Yet it has been shown recently that horizontal gradients can lead to significant errors in satellite infrared and microwave soundings. We extend the methodology to backscatter ultra-violet observations of ozone, and present a first estimate of the effect s magnitude. The Solar Backscatter Ultra-Violet/2 (SBUV/2) instrument, a pure nadir sounder, serves as our test bed. Our results indicate that in a vast majority of cases the abovementioned errors can be neglected. However, occurrence of higher errors, particularly at wavelengths longer than 300 nm, coincides with some of the most interesting atmospheric phenomena like tropopause folds and the South polar ozone hole. This leads to a seasonal variation of the magnitude of the effect. Due to the mostly zonal geometry of the ozone distribution, there is also the possibility that biases may be introduced, which is particularly critical if the data are to be assimilated or used to determine trends. The results presented are tested for robustness using different model atmospheres. The influence of horizontal inhomogeneities will be even more pronounced for cross-track sounders and limb viewers, and easier to detect once higher resolution atmospheric models are available. This will be investigated in future studies.
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- 2005
31. Assimilation Experiments of One-Dimensional Variational Analyses with GPS/MET Refractivity
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Poli, Paul, Joiner, Joanna, and Atlas, Robert
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Aircraft Communications And Navigation - Abstract
The GPS/MET 1995 experiment demonstrated the feasibility of remote soundings of the Earth's atmosphere using the GPS radio occultation technique. Subsequent studies assessed the information content of such measurements. Several groups have attempted to assimilate the GPS radio occultation measurements into a global Data Assimilation System (DAS). These attempts followed in general the methodology proposed by Eyre, and range from die act four-dimensional variational assimilation of bending angles to assimilation of inverted profiles of temperature and/or humidity. We present here an hybrid approach. We attempted to take advantage of the accuracy of current, weather models to constrain one-dimensional variational analyses using GPS refractivity. Retrieved profiles of atmospheric parameters were then assimilated like other types of observations in a global DAS for issuing the next forecast period.
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- 2002
32. Evaluation of Refractivity Profiles From Champ and SAC-C GPS Radio Occultation
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Poli, Paul, Joiner, Joanna, delaTorreJuarez, Manuel, Hoff, Raymond M, and Atlas, Robert
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Aircraft Communications And Navigation - Abstract
The CHAMP and SAC-C missions are the first missions to carry a second-generation 'Blackjack' GPS receiver. One of the new features of this receiver is its ability to sense the lower troposphere closer to the surface than the proof-of-concept GPS/MET 1995 experiment. Since their launch, CHAMP and SAC-C have collected thousands of GPS radio occultations, representing a wealth of measurements available for data assimilation in Numerical Weather Prediction (NWP) models. In order to evaluate the refractivity data derived by JPL from raw radio occultation measurements, we use Data Assimilation Office (DAO) shout forecasts as an independent state of the atmosphere. We compare CHAMP and SAC-C refractivity (processed by JPL) with refractivity calculated from the DAO global fields of temperature, water vapor content and humidity. We will show statistics of the differences as well as Probability Density Functions (PDFs) of the differences. Depending upon availability of AIRS data, we plan to show individual profile comparisons between GPS radio occultation and AIRS retrievals.
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- 2002
33. Temperature Humidity and Sea Level Pressure Increments Induced by 1DVAR Analysis of GPS Refractivity
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Poli, Paul, Joiner, Joanna, Kursinski, Emil Robert, and Einaudi, Franco
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Aircraft Communications And Navigation - Abstract
The Global Positioning System (GPS) transmitted signals are affected by the atmosphere. Using the radio occultation technique, where a receiver is placed on a low-Earth-orbiting platform. it is possible to perform soundings. by measuring the bending angles of the rays. The information can be converted into atmospheric refractivity. We have developed a one dimensional variational (1DVAR) analysis that uses GPS/MET 1995 refractivity and 6-hour FVDAS (Finite Volume Data Assimilation System) forecasts as background information to constrain the retrievals. The analysis increments are defined as 1DVAR minus background temperature, humidity and sea level pressure. Before assimilating the 1DVAR profiles into the FVDAS. the increments need to be understood. First, some bias could be induced in the retrievals when confronted with actual biased data: second. bias in the back-round could create undesired bias in the retrievals. Anv bias in the analyses will ultimately change the climatology of the model the retrievals will be assimilated into. We relate the increments to the reduction of the difference between observed minus computed refractivity profiles. We also point out the difference in the mean increments using backgrounds which have assimilated either NESDIS TIROS Operational Vertical Sounder (TOVS) operational retrievals or Data Assimilation Office (DAO) TOVS interactive retrievals. The climatology of the model in terms of refractivity is significantly different and this impacts the GPS 1DVAR increments. This testifies that changing the basic load of assimilated data has an influence on the impact the GPS data may have in a DAS.
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- 2001
34. A Proposal For Drifting Buoy Metadata In The Wigos Metadata Standard
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Poli, Paul
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ComputingMethodologies_DOCUMENTANDTEXTPROCESSING ,Data_FILES - Abstract
This document proposes a mapping between drifter metadata and the WIGOS metadata standard.
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- 2018
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35. Advancing global & regional reanalyses
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Buizza, Roberto, Poli, Paul, Rixen, Michel, Alonso-Balmaseda, Magdalena, Bosilovich, Michael G., Brönnimann, Stefan, Compo, Gilbert P., Dee, Dick P., Desiato, Franco, Doutriaux-Boucher, Marie, Fujiwara, Masamoto, Kaiser-Weiss, Andrea K., Kobayashi, Shinya, Liu, Zhiquan, Masina, Simona, Mathieu, Pierre-Philippe, Rayner, Nick, Richter, Carolin, Seneviratne, Sonia I., Simmons, Adrian J., Thépaut, Jean-Noel, Auger, Jeffrey D., Bechtold, Michel, Berntell, Ellen, Dong, Bo, Kozubek, Michal, Sharif, Khaled, Thomas, Christopher, Schimanke, Semjon, Storto, Andrea, Tuma, Matthias, Välisuo, Ilona, and Vaselali, Alireza
- Abstract
This report outlines the structure of and summarizes the recommendations made at the 5th International Conference on Reanalysis (ICR5), attended by 259 participants from 37 countries, in Rome (Italy), on 13-17 November 2017. It first summarizes the conference structure. Then, the key recommendations of ICR5 are given for the five main conference topics: production; observations (data rescue and preparation); data assimilation methods; quality assurance of reanalysis; and applications in science, services, and policymaking. Lastly, five high-level recommendations are proposed to managing agencies on how best to advance the field of reanalyses, which serves tens of thousands of users, via enhanced research, development, and operations.
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- 2018
36. Note on the impact of meteorological data from PIRATA moorings on global weather forecasts
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Poli, Paul
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This note analyses the Forecast Sensitivity to Observation results for PIRATA buoy data assimilated in the ECMWF operational numerical weather prediction system.
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- 2018
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37. Drifter network improvement report
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Poli, Paul, Bourles, Bernard, Bond, Steve, Hafner, Sabine, Klink, Stefan, and Petermann, Eric
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14. Life underwater - Abstract
An improvement in drifting buoy coverage is proposed in the South Atlantic, achieved by deployments using ships of opportunity. A study report on benefits of the improved network will be included in this deliverable. Deployments will be coordinated with NOAA (Third party to Ifremer) and Met Office
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- 2018
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38. Atlantic Ocean Observing Networks: Cost and feasibility study
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Reilly, Kieran, Cusack, Caroline, Fernandez, Vicente, Buch, Erik, Ott, Michael, Araujo, Moacyr, Bourles, Bernard, Cancouet, Romain, Connell, Kenneth, Cristini, Luisa, Dolk, Shaun, Edwards, Martin, Emzivat, Gilbert, Fischer, Albert, Fitzhenry, Deirdre, Gourcuff, Claire, Karstensen, Johannes, King, Andrew, Kuska, Gerhard, Lampitt, Richard, Lumpkin, Rick, McDonough, Niall, McPhaden, Mike, Nobre, Paulo, O'Conchubhair, Diarmuid, O'Rourke, Eleanor, Obolensky, Grigor, Piotrowicz, Stephen, Poli, Paul, Pouliquen, Sylvie, Rae, Margaret, Schauer, Ursula, Schuster, Ute, Sloyan, Bernadette, Steventon, Emma, Tanhua, Toste, Tanner, Gil, Testor, Pierre, Trotte, Janice, Turpin, Victor, Turton, Jon, Townsend, Brendal, Wanninkhof, Rik, and Whoriskey, Fred
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14. Life underwater - Abstract
Results of a cost and feasibility study of the present and planned integrated Atlantic Ocean Observing System, including assessing the readiness and feasibility of implementation of different observing technologies
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- 2018
39. Development of Surface Drifting Buoys for Fiducial Reference Measurements of Sea-Surface Temperature
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Le Menn, Marc, primary, Poli, Paul, additional, David, Arnaud, additional, Sagot, Jérôme, additional, Lucas, Marc, additional, O'Carroll, Anne, additional, Belbeoch, Mathieu, additional, and Herklotz, Kai, additional
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- 2019
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40. Global in situ Observations of Essential Climate and Ocean Variables at the Air–Sea Interface
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Centurioni, Luca R., primary, Turton, Jon, additional, Lumpkin, Rick, additional, Braasch, Lancelot, additional, Brassington, Gary, additional, Chao, Yi, additional, Charpentier, Etienne, additional, Chen, Zhaohui, additional, Corlett, Gary, additional, Dohan, Kathleen, additional, Donlon, Craig, additional, Gallage, Champika, additional, Hormann, Verena, additional, Ignatov, Alexander, additional, Ingleby, Bruce, additional, Jensen, Robert, additional, Kelly-Gerreyn, Boris A., additional, Koszalka, Inga M., additional, Lin, Xiaopei, additional, Lindstrom, Eric, additional, Maximenko, Nikolai, additional, Merchant, Christopher J., additional, Minnett, Peter, additional, O’Carroll, Anne, additional, Paluszkiewicz, Theresa, additional, Poli, Paul, additional, Poulain, Pierre-Marie, additional, Reverdin, Gilles, additional, Sun, Xiujun, additional, Swail, Val, additional, Thurston, Sidney, additional, Wu, Lixin, additional, Yu, Lisan, additional, Wang, Bin, additional, and Zhang, Dongxiao, additional
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- 2019
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41. Ship-Based Contributions to Global Ocean, Weather, and Climate Observing Systems
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Smith, Shawn R., primary, Alory, Gaël, additional, Andersson, Axel, additional, Asher, William, additional, Baker, Alex, additional, Berry, David I., additional, Drushka, Kyla, additional, Figurskey, Darin, additional, Freeman, Eric, additional, Holthus, Paul, additional, Jickells, Tim, additional, Kleta, Henry, additional, Kent, Elizabeth C., additional, Kolodziejczyk, Nicolas, additional, Kramp, Martin, additional, Loh, Zoe, additional, Poli, Paul, additional, Schuster, Ute, additional, Steventon, Emma, additional, Swart, Sebastiaan, additional, Tarasova, Oksana, additional, de la Villéon, Loic Petit, additional, and Vinogradova-Shiffer, Nadya, additional
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- 2019
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42. The Joint IOC (of UNESCO) and WMO Collaborative Effort for Met-Ocean Services
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Pinardi, Nadia, primary, Stander, Johan, additional, Legler, David M., additional, O'Brien, Kevin, additional, Boyer, Tim, additional, Cuff, Tom, additional, Bahurel, Pierre, additional, Belbeoch, Mathieu, additional, Belov, Sergey, additional, Brunner, Shelby, additional, Burger, Eugene, additional, Carval, Thierry, additional, Chang-Seng, Denis, additional, Charpentier, Etienne, additional, Ciliberti, S., additional, Coppini, Giovanni, additional, Fischer, Albert, additional, Freeman, Eric, additional, Gallage, Champika, additional, Garcia, Hernan, additional, Gates, Lydia, additional, Gong, Zhiqiang, additional, Hermes, Juliet, additional, Heslop, Emma, additional, Grimes, Sarah, additional, Hill, Katherine, additional, Horsburgh, Kevin, additional, Iona, Athanasia, additional, Mancini, Sebastien, additional, Moodie, Neal, additional, Ouellet, Mathieu, additional, Pissierssens, Peter, additional, Poli, Paul, additional, Proctor, Roger, additional, Smith, Neville, additional, Sun, Charles, additional, Swail, Val, additional, Turton, Jonathan, additional, and Xinyang, Yue, additional
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- 2019
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43. A Global Ocean Observing System (GOOS), Delivered Through Enhanced Collaboration Across Regions, Communities, and New Technologies
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Moltmann, Tim, primary, Turton, Jon, additional, Zhang, Huai-Min, additional, Nolan, Glenn, additional, Gouldman, Carl, additional, Griesbauer, Laura, additional, Willis, Zdenka, additional, Piniella, Ángel Muñiz, additional, Barrell, Sue, additional, Andersson, Erik, additional, Gallage, Champika, additional, Charpentier, Etienne, additional, Belbeoch, Mathieu, additional, Poli, Paul, additional, Rea, Anthony, additional, Burger, Eugene F., additional, Legler, David M., additional, Lumpkin, Rick, additional, Meinig, Christian, additional, O’Brien, Kevin, additional, Saha, Korak, additional, Sutton, Adrienne, additional, Zhang, Dongxiao, additional, and Zhang, Yongsheng, additional
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- 2019
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44. A New Type of DBCP compliant drifting Buoy: the SVP-BRST
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Lucas, Marc, primary, Menn, Marc le, additional, David, Arnaud, additional, Sagot, Jerome, additional, Poli, Paul, additional, Herklotz, Kai, additional, Belbeoch, Mathieu, additional, and O'Carroll, Anne, additional
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- 2019
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45. Towards a Traceable Climate Service: Assessment of Quality and Usability of Essential Climate Variables
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Zeng, Yijian, primary, Su, Zhongbo, additional, Barmpadimos, Iakovos, additional, Perrels, Adriaan, additional, Poli, Paul, additional, Boersma, K. Folkert, additional, Frey, Anna, additional, Ma, Xiaogang, additional, de Bruin, Karianne, additional, Goosen, Hasse, additional, John, Viju O., additional, Roebeling, Rob, additional, Schulz, Jörg, additional, and Timmermans, Wim, additional
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- 2019
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46. Reply to Comment#2
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Poli, Paul, primary
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- 2019
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47. 1DVAR Analysis of Temperature and Humidity using GPS Radio Occulation Data
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Poli, Paul, Joiner, Joanna, Kursinski, Robert, and Kolodner, Marc
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Geophysics - Abstract
The Global Positioning System (GPS) enables positioning with a very small receiver. The signals transmitted by the GPS satellites are sensitive to the atmosphere and can be used to perform soundings with the radio occultation technique (e.g., Kursinski et al., 1997). The GPS signal can be converted to refractivity N via the Abel transform. The refractivity can then be related to atmospheric pressure P, temperature T, and water vapor partial pressure P (sub w) the GPS measurement, (between 0.5 and 1.5 km), its self-calibration, and it's nearly all-weather capabilities make it a good candidate for use in data assimilation systems (DAS) and numerical weather prediction (NWP). In order to demonstrate its usefulness in a DAS or NWP system, a first step is to assess its impact oil the analysis. A one-dimensional variational off-line analysis (1DVAR), meaning the data are not assimilated 'In the 3D DAS, constitutes a starting approach to which further enhancements can be made. The chosen observable to be analyzed in this study is the refractivity. One way to extract temperature (humidity) from the refractivity, is to assume a humidity (temperature) profile. One variable may then be retrieved without any a priori information. The 1DVAR approach used here resolves the ambiguity problem raised in the interpretation of these data. It enables retrieving these two atmospheric variables at a reasonable computing cost.
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- 2000
48. Revisiting the data record of High Resolution Sea Surface Temperature drifting buoys: possible implications for climate monitoring
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Poli, Paul
- Abstract
Between 2012 and 2015, the EIG EUMETNET Operational Service for surface marine observations (E-SURFMAR) and European partners funded and deployed drifting buoys equipped to measure High Resolution Sea Surface Temperature. The HRSST referred to three major improvements as compared to standard practices at the time. First, the positioning accuracy was increased, thanks to GPS instead of Argos. Second, the temperature was transmitted and reported at higher resolution, 0.01 K instead of 0.1 K. Third, each buoy used an individually calibrated temperature probe, instead of one picked from a batch calibration. Note the first two improvements (but not the third) are now standard on most drifting buoys. In addition, some of these buoys were also fitted with two digital probes, one in the buoy hull around 17 cm depth, and another located around 45 cm depth (as part of a conductivity and temperature sensor). This configuration, with two accurate sensors, offered near-optimal horizontal and temporal collocation. The data records from the two sensors, located at different depths, were revisited with the help of reanalysis products as a proxy for the sea-state. The differences between the two sensors can be reduced from 0.21 K RMS to 0.06 K RMS after retaining only the situations that likely correspond to well-mixed SST. Accounting for individual buoy biases, the differences are further reduced to 0.02 K RMS. This would tend to suggest a strong relationship of the relevance of SST measurement with depth and sea-state, and the importance of these factors when using in situ SST data for climate monitoring. Another result concerns potentially the temporal stability of buoy SST data. The HRSST buoys were first calibrated individually in certified laboratories. Three buoys were recovered and the temperature sensors were brought back to a certified laboratory in 2016. Comparing the initial laboratory results with those of 2016, a temporal drift of about 0.01K/year is found for each of the three buoys. These results from so few buoys cannot be claimed to be significant. However, if confirmed, these results would have applications on the use of in situ SST buoy data as a reference, without any temporal drift correction, for the calibration and validation of satellite data and to monitor the climate.
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- 2017
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49. Reply to Comments 1
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Poli, Paul, primary
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- 2018
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50. Southward shift of the northern tropical belt from 1945 to 1980 (vol 8, pg 969, 2015)
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Broennimann Stefan, Fischer Andreas M., Rozanov Eugene, Poli Paul, Compo Gilbert P., and Sardeshmukh Prashant D.
- Abstract
Changes in the position and width of the tropical belt are societally and ecologically relevant because they are associated with shifts of the subtropical dry zones. The tropical belt has widened since about 1980 but little is known about its earlier variability. Here we analyse historical surface and upper level observations three global reanalysis data sets and a reconstruction of total column ozone to show that the northern tropical edge retracted from 1945 to 1980 while the northern Hadley cell shifted southwards in both summer and winter. We present chemistry–climate model simulations that reproduce the retraction and southward shift. We find that retraction of the tropical belt was largely due to cooling sea surface temperatures north of the Equator and warming south of the Equator most prominently over the Atlantic. Substantial hydroclimatic anomalies such as European droughts of the 1940s and 1950s and the Sahel drought of the 1970s were associated with this shift of the Hadley cell. Our results suggest that multidecadal changes in the position of the northern Hadley cell are an important component of climate variability.
- Published
- 2015
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