T
Tasha E. Reddy
Researcher at Stanford University
Publications - 4
Citations - 709
Tasha E. Reddy is an academic researcher from Stanford University. The author has contributed to research in topics: Sea ice & Ocean current. The author has an hindex of 4, co-authored 4 publications receiving 618 citations. Previous affiliations of Tasha E. Reddy include New York University.
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A comparison of global estimates of marine primary production from ocean color
Mary-Elena Carr,Marjorie A. M. Friedrichs,Marjorie A. M. Friedrichs,M. Schmeltz,Maki Noguchi Aita,David Antoine,Kevin R. Arrigo,Ichio Asanuma,Olivier Aumont,Richard T. Barber,Michael J. Behrenfeld,Robert R. Bidigare,Erik T. Buitenhuis,Janet W. Campbell,Áurea Maria Ciotti,Heidi M. Dierssen,Mark Dowell,John P. Dunne,Wayne E. Esaias,Bernard Gentili,Watson W. Gregg,Steve Groom,Nicolas Hoepffner,Joji Ishizaka,Takahiko Kameda,Corinne Le Quéré,Corinne Le Quéré,Steven E. Lohrenz,John Marra,Frédéric Mélin,Keith Moore,André Morel,Tasha E. Reddy,John P. Ryan,Michele Scardi,Timothy J Smyth,Kevin R. Turpie,Gavin H. Tilstone,Kirk Waters,Yasuhiro Yamanaka +39 more
TL;DR: The third primary production algorithm round robin (PPARR3) as discussed by the authors compares output from 24 models that estimate depth-integrated primary production from satellite measurements of ocean color, as well as seven general circulation models (GCMs) coupled with ecosystem or biogeochemical models.
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Ross ice shelf cavity circulation, residence time, and melting: Results from a model of oceanic chlorofluorocarbons
TL;DR: In this article, the authors present results from a modeling study of air-sea chlorofluorocarbon exchange and ocean circulation in the Ross Sea, Antarctica, and compare their model estimates of oceanic CFC-12 concentrations along an ice shelf edge transect to field data collected during three cruises spanning 16 years.
Journal ArticleDOI
Constraints on the extent of the Ross Sea phytoplankton bloom
Tasha E. Reddy,Kevin R. Arrigo +1 more
TL;DR: In this article, the authors present a modeling study indicating that this pattern in the spring phytoplankton bloom is caused by intrusions of offshore surface waters onto the continental shelf, guided by relatively deep polar shelf bathymetry.
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The role of thermal and mechanical processes in the formation of the Ross Sea summer polynya
TL;DR: In this paper, the authors used a three-dimensional coupled ice/ocean model to better understand processes controlling the dynamics of the Ross Sea polynya and found that wind stress plays the primary role in the formation of summer polynyas.