27 results on '"Pallandt, Martijn"'
Search Results
2. Earlier snowmelt may lead to late season declines in plant productivity and carbon sequestration in Arctic tundra ecosystems
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Zona, Donatella, Lafleur, Peter M, Hufkens, Koen, Bailey, Barbara, Gioli, Beniamino, Burba, George, Goodrich, Jordan P, Liljedahl, Anna K, Euskirchen, Eugénie S, Watts, Jennifer D, Farina, Mary, Kimball, John S, Heimann, Martin, Göckede, Mathias, Pallandt, Martijn, Christensen, Torben R, Mastepanov, Mikhail, López-Blanco, Efrén, Jackowicz-Korczynski, Marcin, Dolman, Albertus J, Marchesini, Luca Belelli, Commane, Roisin, Wofsy, Steven C, Miller, Charles E, Lipson, David A, Hashemi, Josh, Arndt, Kyle A, Kutzbach, Lars, Holl, David, Boike, Julia, Wille, Christian, Sachs, Torsten, Kalhori, Aram, Song, Xia, Xu, Xiaofeng, Humphreys, Elyn R, Koven, Charles D, Sonnentag, Oliver, Meyer, Gesa, Gosselin, Gabriel H, Marsh, Philip, and Oechel, Walter C
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Biological Sciences ,Ecology ,Life on Land ,Arctic Regions ,Carbon Dioxide ,Carbon Sequestration ,Climate Change ,Ecosystem ,Plants ,Seasons ,Soil ,Tundra - Abstract
Arctic warming is affecting snow cover and soil hydrology, with consequences for carbon sequestration in tundra ecosystems. The scarcity of observations in the Arctic has limited our understanding of the impact of covarying environmental drivers on the carbon balance of tundra ecosystems. In this study, we address some of these uncertainties through a novel record of 119 site-years of summer data from eddy covariance towers representing dominant tundra vegetation types located on continuous permafrost in the Arctic. Here we found that earlier snowmelt was associated with more tundra net CO2 sequestration and higher gross primary productivity (GPP) only in June and July, but with lower net carbon sequestration and lower GPP in August. Although higher evapotranspiration (ET) can result in soil drying with the progression of the summer, we did not find significantly lower soil moisture with earlier snowmelt, nor evidence that water stress affected GPP in the late growing season. Our results suggest that the expected increased CO2 sequestration arising from Arctic warming and the associated increase in growing season length may not materialize if tundra ecosystems are not able to continue sequestering CO2 later in the season.
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- 2022
3. High‐Latitude Eddy Covariance Temporal Network Design and Optimization.
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Pallandt, Martijn M. T. A., Jung, Martin, Arndt, Kyle, Natali, Susan M., Rogers, Brendan M., Virkkala, Anna‐Maria, and Göckede, Mathias
- Abstract
Ecosystems at high latitudes are changing rapidly in response to climate change. To understand changes in carbon fluxes across seasonal to multi‐decadal timescales, long‐term in situ measurements from eddy covariance networks are needed. However, there are large spatiotemporal gaps in the high‐latitude eddy covariance network. Here we used the relative extrapolation error index in machine learning‐based upscaled gross primary production as a measure of network representativeness and as the basis for a network optimization. We show that the relative extrapolation error index has steadily decreased from 2001 to 2020, suggesting diminishing upscaling errors. In experiments where we limit site activity by either setting a maximum duration or by ending measurements at a fixed time those errors increase significantly, in some cases setting the network status back more than a decade. Our experiments also show that with equal site activity across different theoretical network setups, a more spread out design with shorter‐term measurements functions better in terms of larger‐scale representativeness than a network with fewer long‐term towers. We developed a method to select optimized site additions for a network extension, which blends an objective modeling approach with expert knowledge. This method greatly outperforms an unguided network extension and can compensate for suboptimal human choices. For the Canadian Arctic we show several optimization scenarios and find that especially the Canadian high Arctic and north east tundra benefit greatly from addition sites. Overall, it is important to keep sites active and where possible make the extra investment to survey new strategic locations. Plain Language Summary: The Arctic is one of earth's regions most severely affected by climate change as ice sheets melt and permafrost thaws. This permafrost is rich in carbon which will be released in time. How fast and in which form this carbon is released is highly uncertain. Release as methane would, for example, cause greater global warming in the near future than if it were released as carbon dioxide. It is therefore important to properly measure this carbon release so society can properly prepare for its effects. But as the Arctic is remote and has extreme conditions, there are not so many measuring stations and they might not cover all essential regions. We investigate how well this network represents the Arctic, and where there might be gaps both in space and time. We find that it is essential to keep currently active sites running since if we were to stop measurements our ability to predict this carbon release would not only stagnate but rapidly decline. We developed a method to identify regions that are underrepresented and by incorporating expert knowledge and a new optimization algorithm we can find ideal locations to expand the monitoring network, to better prepare for the future. Key Points: The network of high‐latitude eddy covariance sites has expanded over time, still, sites should remain active and new remote locations addedWhen sites are discontinued, upscaling model skill declines over time, and more quickly in large networksNetwork optimization methods as shown here are a valuable tool to ensure a representative network design [ABSTRACT FROM AUTHOR]
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- 2024
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4. High-latitude eddy covariance temporal network design and optimization.
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Pallandt, Martijn, primary, Jung, Martin, additional, Arndt, Kyle A, additional, Natali, Susan M., additional, Rogers, Brendan, additional, Virkkala, Anna- Maria, additional, and Göckede, Mathias, additional
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- 2023
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5. Temporal factors in the high latitude eddy covariance network design
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Pallandt, Martijn, primary, Jung, Martin, additional, and Goeckede, Mathias, additional
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- 2023
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6. Pan‐Arctic soil moisture control on tundra carbon sequestration and plant productivity
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Zona, Donatella, primary, Lafleur, Peter M., additional, Hufkens, Koen, additional, Gioli, Beniamino, additional, Bailey, Barbara, additional, Burba, George, additional, Euskirchen, Eugénie S., additional, Watts, Jennifer D., additional, Arndt, Kyle A., additional, Farina, Mary, additional, Kimball, John S., additional, Heimann, Martin, additional, Göckede, Mathias, additional, Pallandt, Martijn, additional, Christensen, Torben R., additional, Mastepanov, Mikhail, additional, López‐Blanco, Efrén, additional, Dolman, Albertus J., additional, Commane, Roisin, additional, Miller, Charles E., additional, Hashemi, Josh, additional, Kutzbach, Lars, additional, Holl, David, additional, Boike, Julia, additional, Wille, Christian, additional, Sachs, Torsten, additional, Kalhori, Aram, additional, Humphreys, Elyn R., additional, Sonnentag, Oliver, additional, Meyer, Gesa, additional, Gosselin, Gabriel H., additional, Marsh, Philip, additional, and Oechel, Walter C., additional
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- 2022
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7. Pan‐Arctic soil moisture control on tundra carbon sequestration and plant productivity.
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Zona, Donatella, Lafleur, Peter M., Hufkens, Koen, Gioli, Beniamino, Bailey, Barbara, Burba, George, Euskirchen, Eugénie S., Watts, Jennifer D., Arndt, Kyle A., Farina, Mary, Kimball, John S., Heimann, Martin, Göckede, Mathias, Pallandt, Martijn, Christensen, Torben R., Mastepanov, Mikhail, López‐Blanco, Efrén, Dolman, Albertus J., Commane, Roisin, and Miller, Charles E.
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TUNDRAS ,SOIL moisture ,PLANT productivity ,CARBON sequestration ,ATMOSPHERIC carbon dioxide ,CARBON cycle - Abstract
Long‐term atmospheric CO2 concentration records have suggested a reduction in the positive effect of warming on high‐latitude carbon uptake since the 1990s. A variety of mechanisms have been proposed to explain the reduced net carbon sink of northern ecosystems with increased air temperature, including water stress on vegetation and increased respiration over recent decades. However, the lack of consistent long‐term carbon flux and in situ soil moisture data has severely limited our ability to identify the mechanisms responsible for the recent reduced carbon sink strength. In this study, we used a record of nearly 100 site‐years of eddy covariance data from 11 continuous permafrost tundra sites distributed across the circumpolar Arctic to test the temperature (expressed as growing degree days, GDD) responses of gross primary production (GPP), net ecosystem exchange (NEE), and ecosystem respiration (ER) at different periods of the summer (early, peak, and late summer) including dominant tundra vegetation classes (graminoids and mosses, and shrubs). We further tested GPP, NEE, and ER relationships with soil moisture and vapor pressure deficit to identify potential moisture limitations on plant productivity and net carbon exchange. Our results show a decrease in GPP with rising GDD during the peak summer (July) for both vegetation classes, and a significant relationship between the peak summer GPP and soil moisture after statistically controlling for GDD in a partial correlation analysis. These results suggest that tundra ecosystems might not benefit from increased temperature as much as suggested by several terrestrial biosphere models, if decreased soil moisture limits the peak summer plant productivity, reducing the ability of these ecosystems to sequester carbon during the summer. [ABSTRACT FROM AUTHOR]
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- 2023
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8. Extrapolation error quantification of the Arctic flux network across space and time, with data driven network optimization.
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Pallandt, Martijn, primary, Jung, Martin, additional, Natali, Susan, additional, Rogers, Brendan, additional, Virkkala, Anna, additional, Watts, Jennifer, additional, and Göckede, Mathias, additional
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- 2022
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9. Representativeness assessment of the pan-Arctic eddy covariance site network and optimized future enhancements
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Pallandt, Martijn M. T. A., primary, Kumar, Jitendra, additional, Mauritz, Marguerite, additional, Schuur, Edward A. G., additional, Virkkala, Anna-Maria, additional, Celis, Gerardo, additional, Hoffman, Forrest M., additional, and Göckede, Mathias, additional
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- 2022
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10. Reply on EC1
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Pallandt, Martijn, primary
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- 2021
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11. Reply on RC1
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Pallandt, Martijn, primary
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- 2021
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12. Earlier Snowmelt May Lead to Late Season Declines in Plant Productivity and Carbon Sequestration in Arctic Tundra Ecosystems
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Zona, Donatella, primary, Lafleur, Peter, additional, Hufkens, Koen, additional, Bailey, Barbara, additional, Gioli, Beniamino, additional, Burba, George, additional, Goodrich, Jordan, additional, Liljedahl, Anna, additional, Euskirchen, Eugenie, additional, Watts, Jennifer, additional, Farina, Mary, additional, Kimball, John, additional, Heimann, Martin, additional, Goeckede, Mathias, additional, Pallandt, Martijn, additional, Christensen, Torben, additional, Mastepanov, Mikhail, additional, Lopez-Blanco, Efren, additional, Jackowicz-Korczynski, Marcin, additional, Dolman, Albertus J., additional, Marchesini, Luca Belelli, additional, Commane, Roisin, additional, Wofsy, Steve, additional, Miller, Charles, additional, Lipson, David, additional, Hashemi, Josh, additional, Arndt, Kyle, additional, Kutzbach, Lars, additional, Holl, David, additional, Boike, Julia, additional, Wille, Christian, additional, Sachs, Torsten, additional, Kalhori, Aram, additional, Song, Xia, additional, Xu, Xiaofeng, additional, Humphreys, Elyn, additional, Koven, Charles, additional, Sonnentag, Oliver, additional, Meyer, Gesa, additional, Gosselin, Gabriel, additional, Marsh, Philip, additional, and Oechel, Walter, additional
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- 2021
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13. Representativeness assessment of the pan-Arctic eddy-covariance site network, and optimized future enhancements
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Pallandt, Martijn, primary, Kumar, Jitendra, additional, Mauritz, Marguerite, additional, Schuur, Edward, additional, Virkkala, Anna-Maria, additional, Celis, Gerardo, additional, Hoffman, Forrest, additional, and Göckede, Mathias, additional
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- 2021
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14. Scaling carbon fluxes from eddy covariance sites to globe : Synthesis and evaluation of the FLUXCOM approach
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Jung, Martin, Schwalm, Christopher, Migliavacca, Mirco, Walther, Sophia, Camps-Valls, Gustau, Koirala, Sujan, Anthoni, Peter, Besnard, Simon, Bodesheim, Paul, Carvalhais, Nuno, Chevallier, Frederic, Gans, Fabian, Goll, Daniel S., Haverd, Vanessa, Köhler, Philipp, Ichii, Kazuhito, Jain, Atul K., Liu, Junzhi, Lombardozzi, Danica, Nabel, Julia E.M.S., Nelson, Jacob A., O'Sullivan, Michael, Pallandt, Martijn, Papale, Dario, Peters, Wouter, Pongratz, Julia, Rödenbeck, Christian, Sitch, Stephen, Tramontana, Gianluca, Walker, Anthony, Weber, Ulrich, Reichstein, Markus, Jung, Martin, Schwalm, Christopher, Migliavacca, Mirco, Walther, Sophia, Camps-Valls, Gustau, Koirala, Sujan, Anthoni, Peter, Besnard, Simon, Bodesheim, Paul, Carvalhais, Nuno, Chevallier, Frederic, Gans, Fabian, Goll, Daniel S., Haverd, Vanessa, Köhler, Philipp, Ichii, Kazuhito, Jain, Atul K., Liu, Junzhi, Lombardozzi, Danica, Nabel, Julia E.M.S., Nelson, Jacob A., O'Sullivan, Michael, Pallandt, Martijn, Papale, Dario, Peters, Wouter, Pongratz, Julia, Rödenbeck, Christian, Sitch, Stephen, Tramontana, Gianluca, Walker, Anthony, Weber, Ulrich, and Reichstein, Markus
- Abstract
FLUXNET comprises globally distributed eddy-covariance-based estimates of carbon fluxes between the biosphere and the atmosphere. Since eddy covariance flux towers have a relatively small footprint and are distributed unevenly across the world, upscaling the observations is necessary to obtain global-scale estimates of biosphere-atmosphere exchange. Based on cross-consistency checks with atmospheric inversions, sun-induced fluorescence (SIF) and dynamic global vegetation models (DGVMs), here we provide a systematic assessment of the latest upscaling efforts for gross primary production (GPP) and net ecosystem exchange (NEE) of the FLUXCOM initiative, where different machine learning methods, forcing data sets and sets of predictor variables were employed. Spatial patterns of mean GPP are consistent across FLUXCOM and DGVM ensembles ( at 1 spatial resolution) while the majority of DGVMs show, for 70 of the land surface, values outside the FLUXCOM range. Global mean GPP magnitudes for 2008-2010 from FLUXCOM members vary within 106 and 130 PgC class with the largest uncertainty in the tropics. Seasonal variations in independent SIF estimates agree better with FLUXCOM GPP (mean global pixel-wise) than with GPP from DGVMs (mean global pixel-wise). Seasonal variations in FLUXCOM NEE show good consistency with atmospheric inversion-based net land carbon fluxes, particularly for temperate and boreal regions. Interannual variability of global NEE in FLUXCOM is underestimated compared to inversions and DGVMs. The FLUXCOM version which also uses meteorological inputs shows a strong co-variation in interannual patterns with inversions (for 2001-2010). Mean regional NEE from FLUXCOM shows larger uptake than inversion and DGVM-based estimates, particularly in the tropics with discrepancies of up to several hundred grammes of carbon per square metre per year. These discrepancies can only partly be reconciled by carbon loss pathways that are implicit in inversions but not captured
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- 2020
15. Scaling carbon fluxes from eddy covariance sites to globe: synthesis and evaluation of the FLUXCOM approach
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Jung, Martin, primary, Schwalm, Christopher, additional, Migliavacca, Mirco, additional, Walther, Sophia, additional, Camps-Valls, Gustau, additional, Koirala, Sujan, additional, Anthoni, Peter, additional, Besnard, Simon, additional, Bodesheim, Paul, additional, Carvalhais, Nuno, additional, Chevallier, Frédéric, additional, Gans, Fabian, additional, Goll, Daniel S., additional, Haverd, Vanessa, additional, Köhler, Philipp, additional, Ichii, Kazuhito, additional, Jain, Atul K., additional, Liu, Junzhi, additional, Lombardozzi, Danica, additional, Nabel, Julia E. M. S., additional, Nelson, Jacob A., additional, O'Sullivan, Michael, additional, Pallandt, Martijn, additional, Papale, Dario, additional, Peters, Wouter, additional, Pongratz, Julia, additional, Rödenbeck, Christian, additional, Sitch, Stephen, additional, Tramontana, Gianluca, additional, Walker, Anthony, additional, Weber, Ulrich, additional, and Reichstein, Markus, additional
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- 2020
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16. Deliverable 2.12 Observational gaps revealed by model sensitivity to observations
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Stammer, Detlef, Lyu, Guokun, Pirazzini, Roberta, Naakka, Tuomas, Nygård, Tiina, Vihma, Timo, Pallandt, Martijn, Goeckede, Mathias, and Reum, Friedemann
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Arctic ,Sensitivity ,Gap Analysis ,Ocean Observing Systems ,INTAROS ,Greeen House Gas Observing Systems ,Atmosphere Observing Systems ,Observations - Abstract
To understand the quality of the existing observing system in the Arctic to capture important elements of change over the Arctic we performed a gap analysis with respect to the Arctic Ocean, the Arctic atmosphere and the high-latitude carbon-monitoring network. The main points of the findings are: 1) The ocean observing system: The satellite altimeter system is a critical system to monitor the high-frequency variability. Due to the presence of sea ice in winter time, most of the area can be observed only every 5-10 days, leading to large observing gaps. Closing the gap can be done with new arrays of bottom pressure sensor ssuch as tide gauges or moorings in the ocean bottom. In addition, high-frequency transport measurements are required in the Fram, Davis Straights, the Barents Sea Opening, and north of the Laptev Sea. On the seasonal cycle, bottom pressure observations from GRACE are required to monitor the mass related variability and sea-ice observations are crucial for monitoring the halosteric related variability. On decadal time scales,it is important to have a sufficient hydrographic observing component capable of capturing temperature and salinity changes over the entire Arctic Ocean from the surface to the bottom. New algorithms that can recover sea level from sea ice covered areas may help to improve current satellite altimeter systems,and to improve the ability to monitor the Beaufort Gyre. 2) The atmosphere observing system: The density of the existing radiosonde observation network is not the most critical factor for the quality of T850 forecast. Instead,the results pointed out that stations on small islands in the middle of the Atlantic Ocean are critical for the quality of analysis. The Central Arctic Ocean and the Northern North-Atlantic would prob-ably benefit most from new sounding stations. Efforts to improve the quality of radiosonde observations, especially in Russia, would be very beneficial for the quality of T850 forecasts in the Arctic and sub-Arctic. Current data assimilation systems are probably not adequate to optimally exploit the information from the existing observational network. 3) GHG fluxes observing system: The existing network of pan-Arctic atmospheric monitoring sites provides continuous, well-calibrated observations on atmospheric greenhouse gas mixing ratios, generating basic information to quantify surface-atmosphere greenhouse gas exchange processes for most regions in Canada, Europe and Western Russia; also the Arctic Ocean receives good overall data coverage. Regions showing limited data coverage include the Russian Far East, Western Alaska, and the Eastern Canadian Provinces. Areas where footprint coverage gaps exist seasonally include parts of Western Russia and Central Siberia. Investments in observational infrastructure in any of these areas would be beneficial to increase the overall coverage of the pan-Arctic atmospheric network for greenhouse gases.
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- 2018
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17. Representativeness assessment of the pan- Arctic eddy-covariance site network, and optimized future enhancements.
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Pallandt, Martijn, Kumar, Jitendra, Mauritz, Marguerite, Schuur, Edward, Virkkala, Anna-Maria, Celis, Gerardo, Hoffman, Forrest, and Göckede, Mathias
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CORPORATE profits ,NET losses ,CLIMATE change ,PERMAFROST ,WINTER ,CARBONACEOUS aerosols - Abstract
Large changes in the Arctic carbon balance are expected as warming linked to climate change threatens to destabilize ancient permafrost carbon stocks. The eddy covariance (EC) method is an established technique to quantify net losses and gains of carbon between the biosphere and atmosphere at high spatio-temporal resolution. Over the past decades, a growing network of terrestrial EC tower sites has been established across the Arctic, but a comprehensive assessment of the network's representativeness within the heterogeneous Arctic region is still lacking. This creates additional uncertainties when integrating flux data across sites, for example when upscaling fluxes to constrain pan-Arctic carbon budgets, and changes therein. This study provides an inventory of Arctic (here < = 60° N) EC sites, which has also been made available online (https://cosima.nceas.ucsb.edu/carbon-flux-sites/). Our database currently comprises 120 EC sites, but only 83 are listed as active, and just 25 of these active sites remain operational throughout the winter. To map the representativeness of this EC network, based on 18 bioclimatic and edaphic variables, we evaluated the similarity between environmental conditions observed at the tower locations and those within the larger Arctic study domain. With the majority of sites located in Fennoscandia and Alaska, these regions were assigned the highest level of network representativeness, while large parts of Siberia and patches of Canada were classified as under-represented. This division between regions is further emphasized for wintertime and methane flux data coverage. Across the Arctic, particularly mountainous regions were poorly represented by the current EC observation network. We tested three different strategies to identify new site locations, or upgrades of existing sites, that optimally enhance the representativeness of the current EC network. While 15 new sites can improve the representativeness of the pan-Arctic network by 20 percent, upgrading as few as 10 existing sites to capture methane fluxes, or remain active during wintertime, can improve their respective network coverage by 28 to 33 percent. This targeted network improvement could be shown to be clearly superior to an unguided selection of new sites, therefore leading to substantial improvements in network coverage based on relatively small investments. [ABSTRACT FROM AUTHOR]
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- 2021
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18. Deliverable 2.4 Report on present observing capacities and gaps: Atmosphere
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Tjernström, Michael, Asmi, Eija, Pirazzini, Roberta, Naakka, Tuomas Naakka, O'Connor, Ewan, Sedlar, Joseph, Devasthale, Abhay, Sodemann, Harald, Ahlstrøm, Andreas Peter, Fausto, Robert Schjøtt, Kohnert, Katrin, Serafimovich, Andrei, Sachs, Torsten, Thorne, Peter, Goeckede, Mathias, Pallandt, Martijn, Lappalainen, Hanna K, Mahura, Alexander, Kontu, Anna, Wawrzyniak, Tomasz, Glowacki, Piotr, Sejr, Mikael K., King, Andrew, and Ottersen, Geir
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Arctic ,INTAROS ,Atmosphere Observing Systems ,Assessment - Abstract
This document includes the description and assessment of atmospheric in situ observing systems, data collections and satellite products. On the basis of the assessment, critical knowledge gaps are identified and recommendations to solve them are provided. This document is intended to: − define the current gaps in knowledge in atmospheric fields that are critical for operational weather forecasts, and for the understanding of processes that need to be better represented in climate models. − suggest where the focus in future Arctic atmospheric observations should be.
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- 2018
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19. Representativeness-Based Sampling Network Design for the Arctic
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Hoffman, Forrest M., Kumar, Jitendra, Hargrove, William W., Pallandt, Martijn, and Goeckedei, Mathias
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spatiotemporal, network analysis, representativeness, ecoregions - Abstract
Resource and logistical constraints limit the frequency and extent of environmental observations, particularly in the Arctic, necessitating the development of a systematic sampling strategy to maximize coverage and objectively represent environmental variability at desired scales. Required is a quantitative methodology for stratifying sampling domains, informing site selection, and determining the representativeness of measurement sites and networks. Multivariate spatiotemporal clustering was applied to down-scaled general circulation model results and data for the State of Alaska at 2 km ✕ 2 km resolution to define multiple sets of bioclimatic ecoregions across two decadal time periods. Maps of ecoregions for the present (2000–2009) and future (2090–2099) were produced, showing how combinations of 37 bioclimatic and permafrost characteristics are distributed and how they may shift in the future. Representative sampling locations are identified on present and future ecoregion maps. A representativeness metric was developed, and representativeness maps for eight candidate sampling locations were produced. This metric was used to characterize the environmental similarity of each site. This analysis provides model-inspired insights into optimal sampling strategies, offers a framework for up-scaling measurements, and provides a down-scaling approach for integration of models and measurements. These techniques can be applied at different spatial and temporal scales to meet the needs of individual measurement campaigns. More recently, we have extended this approach to investigate pan-Arctic and tropical forest representativeness, employing remote sensing and other data products, to quantify coverage of spatial heterogeneity from international monitoring and sampling efforts. New results describing global forest site constituency and Arctic sampling regimes will be presented.
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- 2018
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20. Accurate measurements of atmospheric carbon dioxide and methane mole fractions at the Siberian coastal site Ambarchik
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Reum, Friedemann, primary, Göckede, Mathias, additional, Lavric, Jost V., additional, Kolle, Olaf, additional, Zimov, Sergey, additional, Zimov, Nikita, additional, Pallandt, Martijn, additional, and Heimann, Martin, additional
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- 2019
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21. Supplementary material to "Scaling carbon fluxes from eddy covariance sites to globe: Synthesis and evaluation of the FLUXCOM approach"
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Jung, Martin, primary, Schwalm, Christopher, additional, Migliavacca, Mirco, additional, Walther, Sophia, additional, Camps-Valls, Gustau, additional, Koirala, Sujan, additional, Anthoni, Peter, additional, Besnard, Simon, additional, Bodesheim, Paul, additional, Carvalhais, Nuno, additional, Chevallier, Frederic, additional, Gans, Fabian, additional, Groll, Daniel S., additional, Haverd, Vanessa, additional, Ichii, Kazuhito, additional, Jain, Atul K., additional, Liu, Junzhi, additional, Lombardozzi, Danica, additional, Nabel, Julia E. M. S., additional, Nelson, Jacob A., additional, Pallandt, Martijn, additional, Papale, Dario, additional, Peters, Wouter, additional, Pongratz, Julia, additional, Rödenbeck, Christian, additional, Sitch, Stephen, additional, Tramontana, Gianluca, additional, Weber, Ulrich, additional, Reichstein, Markus, additional, Koehler, Philipp, additional, O'Sullivan, Michael, additional, and Walker, Anthony, additional
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- 2019
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22. Scaling carbon fluxes from eddy covariance sites to globe: Synthesis and evaluation of the FLUXCOM approach
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Jung, Martin, primary, Schwalm, Christopher, additional, Migliavacca, Mirco, additional, Walther, Sophia, additional, Camps-Valls, Gustau, additional, Koirala, Sujan, additional, Anthoni, Peter, additional, Besnard, Simon, additional, Bodesheim, Paul, additional, Carvalhais, Nuno, additional, Chevallier, Frederic, additional, Gans, Fabian, additional, Groll, Daniel S., additional, Haverd, Vanessa, additional, Ichii, Kazuhito, additional, Jain, Atul K., additional, Liu, Junzhi, additional, Lombardozzi, Danica, additional, Nabel, Julia E. M. S., additional, Nelson, Jacob A., additional, Pallandt, Martijn, additional, Papale, Dario, additional, Peters, Wouter, additional, Pongratz, Julia, additional, Rödenbeck, Christian, additional, Sitch, Stephen, additional, Tramontana, Gianluca, additional, Weber, Ulrich, additional, Reichstein, Markus, additional, Koehler, Philipp, additional, O'Sullivan, Michael, additional, and Walker, Anthony, additional
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- 2019
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23. Accurate measurements of atmospheric carbon dioxide and methane mole fractions at the Siberian coastal site Ambarchik
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Reum, Friedemann, primary, Göckede, Mathias, additional, Lavric, Jost V., additional, Kolle, Olaf, additional, Zimov, Sergey, additional, Zimov, Nikita, additional, Pallandt, Martijn, additional, and Heimann, Martin, additional
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- 2018
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24. Accurate measurements of atmospheric carbon dioxide and methane mole fractions at the Siberian coastal site Ambarchik.
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Reum, Friedemann, G'ckede, Mathias, Lavric, Jost V., Kolle, Olaf, Zimov, Sergey, Zimov, Nikita, Pallandt, Martijn, and Heimann, Martin
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ATMOSPHERIC carbon dioxide ,CARBON cycle ,CLIMATE change - Abstract
Sparse data coverage in the Arctic hampers our understanding of its carbon cycle dynamics and our predictions of the fate of its vast carbon reservoirs in a changing climate. In this paper, we present accurate measurements of atmospheric CO
2 and CH4 dry air mole fractions at the new atmospheric carbon observation station Ambarchik, which closes a large gap in the atmospheric trace gas monitoring network in northeastern Siberia. The site, operational since August 2014, is located near the delta of the Kolyma River at the coast of the Arctic Ocean. Data quality control of CO2 and CH4 measurements includes frequent calibrations traced to WMO scales, employment of a novel water vapor correction, an algorithm to detect influence of local polluters, and meteorological measurements that enable data selection. The available CO2 and CH4 record was characterized in comparison with in situ data from Barrow, Alaska. A footprint analysis reveals that the station is sensitive to signals from the East Siberian Sea, as well as northeast Siberian tundra and taiga regions. This makes data from Ambarchik highly valuable for inverse modeling studies aimed at constraining carbon budgets within the pan-Arctic domain, as well as for regional studies focusing on Siberia and the adjacent shelf areas of the Arctic Ocean. [ABSTRACT FROM AUTHOR]- Published
- 2018
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25. Scaling carbon fluxes from eddy covariance sites to globe: Synthesis and evaluation of the FLUXCOM approach
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Jung, Martin, Schwalm, Christopher, Migliavacca, Mirco, Walther, Sophia, Camps-Valls, Gastau, Koirala, Sujan, Anthoni, Peter, Besnard, Simon, Bodesheim, Paul, Carvalhais, Nuno, Chevallier, Frederic, Gans, Fabian, Groll, Daniel S., Haverd, Vanessa, Ichii, Kazuhito, Jain, Atul K., Liu, Junzhi, Lombardozzi, Danica, Nabel, Julia E. M. S., Nelson, Jacob A., Pallandt, Martijn, Papale, Dario, Peters, Wouter, Pongratz, Julia, Rödenbeck, Christian, Sitch, Stephen, Tramontana, Gianluca, Weber, Ulrich, Reichstein, Markus, Koehler, Philipp, O’Sullivan, Michael, and Walker, Anthony
- Subjects
13. Climate action ,15. Life on land
26. Evaluation of the pan-Arctic ecosystem scale greenhouse gas monitoring network.
- Author
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Pallandt, Martijn, Göckede, Mathias, Kumar, Jitendru, Martin jung, and Zona, Donatella
- Subjects
- *
GREENHOUSE gases , *ECOSYSTEMS - Published
- 2018
27. Where Do Early Career Researchers Stand on Open Science Practices? A Survey Within the Max Planck Society.
- Author
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Toribio-Flórez D, Anneser L, deOliveira-Lopes FN, Pallandt M, Tunn I, and Windel H
- Abstract
Open science (OS) is of paramount importance for the improvement of science worldwide and across research fields. Recent years have witnessed a transition toward open and transparent scientific practices, but there is still a long way to go. Early career researchers (ECRs) are of crucial relevance in the process of steering toward the standardization of OS practices, as they will become the future decision makers of the institutional change that necessarily accompanies this transition. Thus, it is imperative to gain insight into where ECRs stand on OS practices. Under this premise, the Open Science group of the Max Planck PhDnet designed and conducted an online survey to assess the stance toward OS practices of doctoral candidates from the Max Planck Society. As one of the leading scientific institutions for basic research worldwide, the Max Planck Society provides a considerable population of researchers from multiple scientific fields, englobed into three sections: biomedical sciences, chemistry, physics and technology, and human and social sciences. From an approximate total population of 5,100 doctoral candidates affiliated with the Max Planck Society, the survey collected responses from 568 doctoral candidates. The survey assessed self-reported knowledge, attitudes, and implementation of different OS practices, namely, open access publications, open data, preregistrations, registered reports, and replication studies. ECRs seemed to hold a generally positive view toward these different practices and to be interested in learning more about them. Furthermore, we found that ECRs' knowledge and positive attitudes predicted the extent to which they implemented these OS practices, although levels of implementation were rather low in the past. We observed differences and similarities between scientific sections. We discuss these differences in terms of need and feasibility to apply these OS practices in specific scientific fields, but additionally in relation to the incentive systems that shape scientific communities. Lastly, we discuss the implications that these results can have for the training and career advancement of ECRs, and ultimately, for the consolidation of OS practices., Competing Interests: The authors declare that the research was conducted in the absence of any commercial or financial relationships that could be construed as a potential conflict of interest., (Copyright © 2021 Toribio-Flórez, Anneser, deOliveira-Lopes, Pallandt, Tunn and Windel.)
- Published
- 2021
- Full Text
- View/download PDF
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