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6. Priorities for Wind-Waves Research

Author

Greenslade, Diana, Hemer, Mark, Babanin, Alex, Lowe, Ryan, Turner, Ian, Power, Hannah, Young, Ian, Ierodiaconou, Daniel, Hibbert, Greg, Williams, Greg, Aijaz, Saima, Albuquerque, João, Allen, Stewart, Banner, Michael, Branson, Paul, Buchan, Steve, Burton, Andrew, Bye, John, Cartwright, Nick, Chabchoub, Amin, Colberg, Frank, Contardo, Stephanie, Dufois, Francois, Earl-Spurr, Craig, Farr, David, Goodwin, Ian, Gunson, Jim, Hansen, Jeff, Hanslow, David, Harley, Mitchell, Hetzel, Yasha, Hoeke, Ron, Jones, Nicole, Kinsela, Michael, Liu, Qingxiang, Makarynskyy, Oleg, Marcollo, Hayden, Mazaheri, Said, McConochie, Jason, Millar, Grant, Moltmann, Tim, Moodie, Neal, Morim, Joao, Morison, Russel, Orszaghova, Jana, Pattiaratchi, Charitha, Pomeroy, Andrew, Proctor, Roger, Provis, David, Reef, Ruth, Rijnsdorp, Dirk, Rutherford, Martin, Schulz, Eric, Shayer, Jake, Splinter, Kristen, Steinberg, Craig, Strauss, Darrell, Stuart, Greg, Symonds, Graham, Tarbath, Karina, Taylor, Daniel, Taylor, James, Thotagamuwage, Darshani, Toffoli, Alessandro, Valizadeh, Alireza, van Hazel, Jonathan, da Silva, Guilherme Vieira, Wandres, Moritz, Whittaker, Colin, Williams, David, Winter, Gundula, Xu, Jiangtao, Zhong, Aihong, and Zieger, Stefan

Published
2020

7. 15 Priorities for Wind-Waves Research : An Australian Perspective

Author

Greenslade, Diana, Hemer, Mark, Babanin, Alex, Lowe, Ryan, Turner, Ian, Power, Hannah, Young, Ian, Ierodiaconou, Daniel, Hibbert, Greg, Williams, Greg, Aijaz, Saima, Albuquerque, João, Allen, Stewart, Banner, Michael, Branson, Paul, Buchan, Steve, Burton, Andrew, Bye, John, Cartwright, Nick, Chabchoub, Amin, Colberg, Frank, Contardo, Stephanie, Dufois, Francois, Earl-Spurr, Craig, Farr, David, Goodwin, Ian, Gunson, Jim, Hansen, Jeff, Hanslow, David, Harley, Mitchell, Hetzel, Yasha, Hoeke, Ron, Jones, Nicole, Kinsela, Michael, Liu, Qingxiang, Makarynskyy, Oleg, Marcollo, Hayden, Mazaheri, Said, McConochie, Jason, Millar, Grant, Moltmann, Tim, Moodie, Neal, Morim, Joao, Morison, Russel, Orszaghova, Jana, Pattiaratchi, Charitha, Pomeroy, Andrew, Proctor, Roger, Provis, David, Reef, Ruth, Rijnsdorp, Dirk, Rutherford, Martin, Schulz, Eric, Shayer, Jake, Splinter, Kristen, Steinberg, Craig, Strauss, Darrell, Stuart, Greg, Symonds, Graham, Tarbath, Karina, Taylor, Daniel, Taylor, James, Thotagamuwage, Darshani, Toffoli, Alessandro, Valizadeh, Alireza, van Hazel, Jonathan, da Silva, Guilherme Vieira, Wandres, Moritz, Whittaker, Colin, Williams, David, Winter, Gundula, Xu, Jiangtao, Zhong, Aihong, and Zieger, Stefan

Published
2020

8. Links between the three-dimensional movements of whale sharks (Rhincodon typus) and the bio-physical environment off a coral reef.

Author

D'Antonio, Ben, Ferreira, Luciana C., Meekan, Mark, Thomson, Paul G., Lieber, Lilian, Virtue, Patti, Power, Chloe, Pattiaratchi, Charitha B., Brierley, Andrew S., Sequeira, Ana M. M., and Thums, Michele

Subjects
WHALE shark, CORAL reefs & islands, CORALS, PREDATORY aquatic animals, CHLOROPHYLL spectra
Abstract

Background: Measuring coastal-pelagic prey fields at scales relevant to the movements of marine predators is challenging due to the dynamic and ephemeral nature of these environments. Whale sharks (Rhincodon typus) are thought to aggregate in nearshore tropical waters due to seasonally enhanced foraging opportunities. This implies that the three-dimensional movements of these animals may be associated with bio-physical properties that enhance prey availability. To date, few studies have tested this hypothesis. Methods: Here, we conducted ship-based acoustic surveys, net tows and water column profiling (salinity, temperature, chlorophyll fluorescence) to determine the volumetric density, distribution and community composition of mesozooplankton (predominantly euphausiids and copepods) and oceanographic properties of the water column in the vicinity of whale sharks that were tracked simultaneously using satellite-linked tags at Ningaloo Reef, Western Australia. Generalised linear mixed effect models were used to explore relationships between the 3-dimensional movement behaviours of tracked sharks and surrounding prey fields at a spatial scale of ~ 1 km. Results: We identified prey density as a significant driver of horizontal space use, with sharks occupying areas along the reef edge where densities were highest. These areas were characterised by complex bathymetry such as reef gutters and pinnacles. Temperature and salinity profiles revealed a well-mixed water column above the height of the bathymetry (top 40 m of the water column). Regions of stronger stratification were associated with reef gutters and pinnacles that concentrated prey near the seabed, and entrained productivity at local scales (~ 1 km). We found no quantitative relationship between the depth use of sharks and vertical distributions of horizontally averaged prey density. Whale sharks repeatedly dove to depths where spatially averaged prey concentration was highest but did not extend the time spent at these depth layers. Conclusions: Our work reveals previously unrecognized complexity in interactions between whale sharks and their zooplankton prey. [ABSTRACT FROM AUTHOR]

Published
2024
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9. Water properties and bottom water patterns in hadal trench environments.

Author

Kolbusz, Jessica, Zika, Jan, Pattiaratchi, Charitha, and Jamieson, Alan

Subjects
BOTTOM water (Oceanography), TRENCHES, SALINE waters, DEPTH profiling, PORE water
Abstract

We examine baseline water properties and bottom water patterns in hadal trench environments across the Southern Ocean, Indian Ocean, and western Pacific. Significant differences are identified in the South Fiji Basin and surrounding the Philippine Sea, primarily due to the movement of cold Lower Circumpolar Deep Water along topographic features, highlighting the importance of a trench's geospatial position. We present the first hydrographic profiles in the Java Trench, warranting further research. Salinity increases with increasing depth for profiles over 10 000 dbar, with potential causes including instrumentation error, internal mixing, and saline pore water expulsion. These hadopelagic variations are crucial for assessing climate change impacts, especially regarding Antarctic Bottom Water. The study underscores the importance of incorporating these adiabatic conditions to gain insights into ecological biodiversity, alongside the indispensable baseline conditions presented, which are crucial for future oceanographic research across multiple disciplines. [ABSTRACT FROM AUTHOR]

Published
2024
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10. The cycle of seagrass life: From flowers to new meadows

Author

Kendrick, Gary A., primary, Cambridge, Marion L., additional, Orth, Robert J., additional, Fraser, Matthew W., additional, Hovey, Renae K., additional, Statton, John, additional, Pattiaratchi, Charitha B., additional, and Sinclair, Elizabeth A., additional

Published
2023
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12. Ocean circulation around Sri Lanka

Author

Pattiaratchi, Charitha and Wijeratne, Sarath

Abstract

Sri Lanka, located in the northern Indian Ocean with the Arabian Sea on its western side and the Bay of Bengal on its eastern side and experiences bi-annually reversing monsoon winds. This will explore the dynamics of the surface circulation and coastal upwelling in the waters around Sri Lanka, particularly along the southern coast, using satellite imagery and numerical simulations using the Regional Ocean Modelling System (ROMS). The results confirmed the presence of the reversing current system, between the equator and Sri Lanka, in response to the changing wind field: the eastward flowing Southwest Monsoon Current (SMC) during the Southwest (SW) monsoon and the westward flowing Northeast Monsoon Current (NMC) during the Northeast (NE) monsoon, respectively. Along the eastern and western coasts, during both monsoon periods, flow is southward converging along the south coast. During the SW monsoon, along the west coast, the Island deflects the eastward flowing SMC southward whilst along the east coast the southward flow results from the Sri Lanka Dome (SLD) recirculation. SLD is formed due to SMC interation with the Island. The major upwelling region was located along the south coast due to water convergence and subsequent divergence associated with the offshore transport of water. The location of the flow convergence and hence the upwelling centre was dependent on the relative strengths of wind driven flow along the east and west coasts: during the SW (NE) monsoon the flow along the western (eastern) coast was stronger migrating the upwelling centre to the east (west).&nbsp, The 28th IUGG General Assembly (IUGG2023) (Berlin 2023)

Published
2023

16. Introduction to 'Sixty Years of Modern Tsunami Science, Volume 2: Challenges'

Author

KANOĞLU, UTKU, Catalán, Patricio A., Zamora, Natalia, Baptista, Maria Ana, Pattiaratchi, Charitha, Okal, Emile A., and Rabinovich, Alexander B.

Abstract

Fifteen papers are included in this PAGEOPH topical issue “Sixty Years of Modern Tsunami Science, Volume 2: Challenges.” The issue starts with a general introduction, and then briefly summarizes all contributions, first papers addressing general topics, and then articles grouped on a regional basis: Northern Pacific, Southeast Pacific, Southwest Pacific and Indonesia, and Mediterranean regions.

Published
2023

20. Meteorological and volcanic tsunami signals generated by the Hunga Tonga-hunga Ha’apai eruption

Author

Wijeratne, Sarath and Pattiaratchi, Charitha

Abstract

An eruption of the Hunga Tonga-hunga Ha’apai Volcanic Eruption on 15 January 2012 caused tsunami waves, observed globally in tide gage records. In this study we investigate the origin of tsunami waves through the analysis of tide gauge records and numerical simulations in the Indo-Pacific region. The atmospheric pressure wave (Lamb wave) due the eruption was recorded in meteorological stations across Australia. The moving pressure jump was recorded as a ~6.5-hPa jump at the Norfolk Island; ~3.5 hPa at Broken Hill, NSW and Perth and was estimated to be travelling at ~340 ms–1. In the deep ocean this allows for Proudman resonance between the ocean and atmosphere generating a meteotsunami propagating westward across the Indian Ocean. Tide gauges located across the whole Indian Ocean basin recorded the meteotsunami generated by the pressure jump. There were two distinct signal on the tide gauge records. The first signal was recorded in advance of the predicted volcanic tsunami along the east coast of Australia and was due to the meteotsunami. The arrival of the second signal corresponded to tsunami wave generated by the displacement of the volcano travelling as a ‘free’ wave. These findings were confirmed by numerical simulations using an ocean circulation model that incorporated a moving atmospheric pressure jump travelling at a speed of ~ 340 ms–1. The long ocean waves were amplified due to Proudman resonance in the deep ocean, where the water was deeper than 5000 m. The model predicted of the meteotsunami corresponded well with observations., The 28th IUGG General Assembly (IUGG2023) (Berlin 2023)

Published
2023

21. Spatial and temporal variability and vertical structure of mesoscale eddies off Western Australia

Author

Kodithuwakku, Sharani, Pattiaratchi, Charitha, Cosoli, Simone, and Hetzel, Yasha

Abstract

Mesoscale eddies are common physical features in the ocean that are important for the transport of heat and momentum, and for the distribution of biochemical materials in the ocean. The existence of an anomalous, poleward flowing surface current, the Leeuwin Current (LC), drives the highest eddy kinetic energy environment among all the global eastern boundary currents off Western Australia (WA). There is a limitation in comprehensive understanding of spatial and temporal variability, in particular, the formation and vertical structure of mesoscale eddies. Therefore, this study aimed to define the climatology and vertical structure of mesoscale eddies off WA. Eddy characteristics were derived off WA (10‒40ºS, 105‒130ºE) using a vector geometry-based eddy detection algorithm applied to daily satellite altimetry data over the period 1993-2020. The vertical structure of cyclonic eddies (CE) and anti-cyclonic eddies (AE) in the Perth canyon were examined using ocean glider data over the period 2010-2017 obtained from the Australian Integrated Marine Observing System (IMOS). The seasonal and inter-annual variability and the lifecycles of mesoscale eddies were documented off WA. Shorter-lived eddy formations (, The 28th IUGG General Assembly (IUGG2023) (Berlin 2023)

Published
2023

22. Interannual variability of sub-mesoscale eddy distribution and characteristics along Rottnest Continental Shelf, Western Australia: Response to Leeuwin Current variability

Author

Paranhos Bitencourt, Liliane, Pattiaratchi, Charitha, Cosoli, Simone, and Hetzel, Yasha

Abstract

In the eastern margin of the Indian Ocean, anomalous poleward-flowing Leeuwin Current (LC) interacts with the local circulation and topographic features along its path promoting instabilities and a highly energetic eddy field. Eddies play a major role on transferring physical and biogeochemical properties over a wide range of spatial and temporal scales. In particular, sub-mesoscale eddies (SME) are believed to intensify vertical fluxes and are crucial for energy transport. However, as continuous high spatial and temporal resolution data are essential for SME characterization due to their short lifespans and length scale, they are still poorly understood. Thus, this research aims to analyse the spatiotemporal variability of sub-mesoscale eddies distribution and characteristics as a response of LC dynamics along the Rottnest Continental Shelf (ROT). We applied an eddy detection and tracking algorithm to long-term (2010-2018) surface current observations obtained using High-Frequency Radar. LC interactions with the Capes Current and offshore eddies promoted zones with high horizontal shear that were linked to SME generation regions. Counter-clockwise (AC) and clockwise (C) SME were prevalent at the eastern and western boundaries of the LC, respectively, remaining close to their generation spots with 25-50h lifespans. Most of AC (C) SME were formed in August (September). AC eddies generation hotspots migrated meridionally with season, whilst C eddies were clustered in a preferential location, but migrated counter-clockwise over the seasons. The analysis of the long-time series provided detailed information of the generation and lifespans of sub-meso scale eddies and their variability in time in the study region., The 28th IUGG General Assembly (IUGG2023) (Berlin 2023)

Published
2023

25. OceanGliders Oxygen SOP v1.0.0. [GOOS ENDORSED PRACTICE]

Author

Lopez-Garcia, Patricia, Hull, Tom, Thomsen, Soeren, Hahn, Johannes, Queste, Bastien Y., Krahmann, Gerd, Williams, Charlotte, Woo, Mun, Pattiaratchi, Charitha, Coppola, Laurent, Morales, Tania, Racapé, Virginie, Gourcuff, Claire, Allen, John, Alou-Font, Eva, Zarokanellos, Nikolaos D., Turpin, Victor, Schmechtig, Catherine, Testor, Pierre, Busecke, Julius, Bourma, Evi, Richards, Clark, Pearce, Stuart, Carvalho, Filipa, Giddy, Isabelle, and Begler, Christian

Subjects
Data processing, Oxygen, Dissolved gases, Data analysis, Data acquisition, Dissolved gas sensors, Essential Ocean Variables (EOV), EuroSea Project, GeneralLiterature_MISCELLANEOUS
Abstract

The live version of this SOP is on the Ocean Gliders community in GITHUB. The home repository of this publication is in the Ocean Best Practices Repository. This standard operating procedure (SOP) document for dissolved oxygen (DO) aims to guide the user through the steps necessary to collect good quality dissolved oxygen data using ocean gliders for both real time and post deployment data streams.

Published
2022

35. Corrigendum: OceanGliders: A Component of the Integrated GOOS

Author

Testor, Pierre, primary, Young, Brad de, additional, Rudnick, Daniel L., additional, Glenn, Scott, additional, Hayes, Daniel, additional, Lee, Craig M., additional, Pattiaratchi, Charitha, additional, Hill, Katherine, additional, Heslop, Emma, additional, Turpin, Victor, additional, Alenius, Pekka, additional, Barrera, Carlos, additional, Barth, John A., additional, Beaird, Nicholas, additional, Bécu, Guislain, additional, Bosse, Anthony, additional, Bourrin, François, additional, Brearley, J. Alexander, additional, Chao, Yi, additional, Chen, Sue, additional, Chiggiato, Jacopo, additional, Coppola, Laurent, additional, Crout, Richard, additional, Cummings, James, additional, Curry, Beth, additional, Curry, Ruth, additional, Davis, Richard, additional, Desai, Kruti, additional, DiMarco, Steve, additional, Edwards, Catherine, additional, Fielding, Sophie, additional, Fer, Ilker, additional, Frajka-Williams, Eleanor, additional, Gildor, Hezi, additional, Goni, Gustavo, additional, Gutierrez, Dimitri, additional, Haugan, Peter, additional, Hebert, David, additional, Heiderich, Joleen, additional, Henson, Stephanie, additional, Heywood, Karen, additional, Hogan, Patrick, additional, Houpert, Loïc, additional, Huh, Sik, additional, Inall, Mark E., additional, Ishii, Masso, additional, Ito, Shin-ichi, additional, Itoh, Sachihiko, additional, Jan, Sen, additional, Kaiser, Jan, additional, Karstensen, Johannes, additional, Kirkpatrick, Barbara, additional, Klymak, Jody, additional, Kohut, Josh, additional, Krahmann, Gerd, additional, Krug, Marjolaine, additional, McClatchie, Sam, additional, Marin, Frédéric, additional, Mauri, Elena, additional, Mehra, Avichal, additional, Meredith, Michael P., additional, Meunier, Thomas, additional, Miles, Travis, additional, Morell, Julio M., additional, Mortier, Laurent, additional, Nicholson, Sarah, additional, O'Callaghan, Joanne, additional, O'Conchubhair, Diarmuid, additional, Oke, Peter, additional, Pallàs-Sanz, Enric, additional, Palmer, Matthew, additional, Park, JongJin, additional, Perivoliotis, Leonidas, additional, Poulain, Pierre-Marie, additional, Perry, Ruth, additional, Queste, Bastien, additional, Rainville, Luc, additional, Rehm, Eric, additional, Roughan, Moninya, additional, Rome, Nicholas, additional, Ross, Tetjana, additional, Ruiz, Simon, additional, Saba, Grace, additional, Schaeffer, Amandine, additional, Schönau, Martha, additional, Schroeder, Katrin, additional, Shimizu, Yugo, additional, Sloyan, Bernadette M., additional, Smeed, David, additional, Snowden, Derrick, additional, Song, Yumi, additional, Swart, Sebastian, additional, Tenreiro, Miguel, additional, Thompson, Andrew, additional, Tintore, Joaquin, additional, Todd, Robert E., additional, Toro, Cesar, additional, Venables, Hugh, additional, Wagawa, Taku, additional, Waterman, Stephanie, additional, Watlington, Roy A., additional, and Wilson, Doug, additional

Published
2021
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38. Beaching patterns of plastic debris along the Indian Ocean rim

Author

Van Der Mheen, Mirjam, Van Sebille, Erik, Pattiaratchi, Charitha, Sub Physical Oceanography, Marine and Atmospheric Research, Sub Physical Oceanography, and Marine and Atmospheric Research

Subjects
0106 biological sciences, 010504 meteorology & atmospheric sciences, Equator, 010501 environmental sciences, Monsoon, Oceanography, 01 natural sciences, 03 medical and health sciences, Ocean gyre, 14. Life underwater, Southern Hemisphere, lcsh:Environmental sciences, 0105 earth and related environmental sciences, 030304 developmental biology, lcsh:GE1-350, geography, 0303 health sciences, geography.geographical_feature_category, Great Pacific garbage patch, 010604 marine biology & hydrobiology, Palaeontology, lcsh:Geography. Anthropology. Recreation, Debris, Ocean dynamics, lcsh:G, 13. Climate action, Bay, Geology
Abstract

A large percentage of global ocean plastic waste enters the northern hemisphere Indian Ocean (NIO). Despite this, it is unclear what happens to buoyant plastics in the NIO. Because the subtropics in the NIO is blocked by landmass, there is no subtropical gyre and no associated subtropical garbage patch in this region. We therefore hypothesise that plastics "beach" and end up on coastlines along the Indian Ocean rim. In this paper, we determine the influence of beaching plastics by applying different beaching conditions to Lagrangian particle tracking simulation results. Our results show that a large amount of plastic likely ends up on coastlines in the NIO, while some crosses the equator into the southern hemisphere Indian Ocean (SIO). In the NIO, the transport of plastics is dominated by seasonally reversing monsoonal currents, which transport plastics back and forth between the Arabian Sea and the Bay of Bengal. All buoyant plastic material in this region beaches within a few years in our simulations. Countries bordering the Bay of Bengal are particularly heavily affected by plastics beaching on coastlines. This is a result of both the large sources of plastic waste in the region, as well as ocean dynamics which concentrate plastics in the Bay of Bengal. During the intermonsoon period following the southwest monsoon season (September, October, November), plastics can cross the equator on the eastern side of the NIO basin into the SIO. Plastics that escape from the NIO into the SIO beach on eastern African coastlines and islands in the SIO or enter the subtropical SIO garbage patch.

Published
2020

48. Enhancing the Scientific Value of Industry Remotely Operated Vehicles (ROVs) in Our Oceans

Author

McLean, Dianne L., primary, Parsons, Miles J. G., additional, Gates, Andrew R., additional, Benfield, Mark C., additional, Bond, Todd, additional, Booth, David J., additional, Bunce, Michael, additional, Fowler, Ashley M., additional, Harvey, Euan S., additional, Macreadie, Peter I., additional, Pattiaratchi, Charitha B., additional, Rouse, Sally, additional, Partridge, Julian C., additional, Thomson, Paul G., additional, Todd, Victoria L. G., additional, and Jones, Daniel O. B., additional

Published
2020
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50. OceanGliders: A Component of the Integrated GOOS

Author

Testor, Pierre, primary, de Young, Brad, additional, Rudnick, Daniel L., additional, Glenn, Scott, additional, Hayes, Daniel, additional, Lee, Craig M., additional, Pattiaratchi, Charitha, additional, Hill, Katherine, additional, Heslop, Emma, additional, Turpin, Victor, additional, Alenius, Pekka, additional, Barrera, Carlos, additional, Barth, John A., additional, Beaird, Nicholas, additional, Bécu, Guislain, additional, Bosse, Anthony, additional, Bourrin, François, additional, Brearley, J. Alexander, additional, Chao, Yi, additional, Chen, Sue, additional, Chiggiato, Jacopo, additional, Coppola, Laurent, additional, Crout, Richard, additional, Cummings, James, additional, Curry, Beth, additional, Curry, Ruth, additional, Davis, Richard, additional, Desai, Kruti, additional, DiMarco, Steve, additional, Edwards, Catherine, additional, Fielding, Sophie, additional, Fer, Ilker, additional, Frajka-Williams, Eleanor, additional, Gildor, Hezi, additional, Goni, Gustavo, additional, Gutierrez, Dimitri, additional, Haugan, Peter, additional, Hebert, David, additional, Heiderich, Joleen, additional, Henson, Stephanie, additional, Heywood, Karen, additional, Hogan, Patrick, additional, Houpert, Loïc, additional, Huh, Sik, additional, E. Inall, Mark, additional, Ishii, Masso, additional, Ito, Shin-ichi, additional, Itoh, Sachihiko, additional, Jan, Sen, additional, Kaiser, Jan, additional, Karstensen, Johannes, additional, Kirkpatrick, Barbara, additional, Klymak, Jody, additional, Kohut, Josh, additional, Krahmann, Gerd, additional, Krug, Marjolaine, additional, McClatchie, Sam, additional, Marin, Frédéric, additional, Mauri, Elena, additional, Mehra, Avichal, additional, P. Meredith, Michael, additional, Meunier, Thomas, additional, Miles, Travis, additional, Morell, Julio M., additional, Mortier, Laurent, additional, Nicholson, Sarah, additional, O'Callaghan, Joanne, additional, O'Conchubhair, Diarmuid, additional, Oke, Peter, additional, Pallàs-Sanz, Enric, additional, Palmer, Matthew, additional, Park, JongJin, additional, Perivoliotis, Leonidas, additional, Poulain, Pierre-Marie, additional, Perry, Ruth, additional, Queste, Bastien, additional, Rainville, Luc, additional, Rehm, Eric, additional, Roughan, Moninya, additional, Rome, Nicholas, additional, Ross, Tetjana, additional, Ruiz, Simon, additional, Saba, Grace, additional, Schaeffer, Amandine, additional, Schönau, Martha, additional, Schroeder, Katrin, additional, Shimizu, Yugo, additional, Sloyan, Bernadette M., additional, Smeed, David, additional, Snowden, Derrick, additional, Song, Yumi, additional, Swart, Sebastian, additional, Tenreiro, Miguel, additional, Thompson, Andrew, additional, Tintore, Joaquin, additional, Todd, Robert E., additional, Toro, Cesar, additional, Venables, Hugh, additional, Wagawa, Taku, additional, Waterman, Stephanie, additional, Watlington, Roy A., additional, and Wilson, Doug, additional

Published
2019
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