Zobrazeno 1 - 10
of 14
pro vyhledávání: '"Deepak Cherian"'
Autor:
James N. Moum, William D. Smyth, Kenneth G. Hughes, Deepak Cherian, Sally J. Warner, Bernard Bourlès, Peter Brandt, Marcus Dengler
Publikováno v:
Journal of Physical Oceanography.
Several years of moored turbulence measurements from χpods at three sites in the equatorial cold tongues of Atlantic and Pacific Oceans yield new insights into proxy estimates of turbulence that specifically target the cold tongues. They also reveal
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::053d8f4d1344ea6d82c81fe11ada9882
https://doi.org/10.1175/jpo-d-22-0203.1
https://doi.org/10.1175/jpo-d-22-0203.1
Autor:
Arnold L. Gordon, E. Creegan, Jaynise Pérez, Adam V. Rydbeck, Rashmi Sharma, Uwe Send, Maria Flatau, Verena Hormann, Craig M. Lee, Hemantha W. Wijesekera, G. S. Bhat, Michael J. McPhaden, Rajib Chattopadhyay, Luca Centurioni, Bulusu Subrahmanyam, Arachaporn Anutaliya, Simon P. de Szoeke, Ramasamy Venkatesan, Deepak Cherian, Jennifer A. MacKinnon, S. U. P. Jinadasa, Jossia Joseph, Andrew Lucas, Luc Rainville, Kaitlyn M. Woods, Harindra J. S. Fernando, Manikandan Mathur, Hyodae Seo, M. Mohapatra, Shannon M. Bohman, Gad Levy, A. K. Sahai, Matthias Lankhorst, Robert E. Todd, Lakshmi Kantha, Tamara Schlosser, E. Pattabhi Rama Rao, K. Adams, Emily L. Shroyer, Garrett S. Black, Amy F. Waterhouse, Steven R. Jayne, S. Ramsundaram, Amit Tandon, Iury T. Simoes-Sousa, Aneesh C. Subramanian, J. Thomas Farrar, Kerstin Cullen, Jeremy A. Dehart, Debasis Sengupta
Publikováno v:
Bulletin of the American Meteorological Society. 102:E1936-E1951
In the Bay of Bengal, the warm, dry boreal spring concludes with the onset of the summer monsoon and accompanying southwesterly winds, heavy rains, and variable air–sea fluxes. Here, we summarize the 2018 monsoon onset using observations collected
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::bf2d700cd8c8beb21bfb59b23c6171ad
https://doi.org/10.1175/bams-d-20-0113.1
https://doi.org/10.1175/bams-d-20-0113.1
Autor:
Ren-Chieh Lien, William G. Large, Daniel B. Whitt, Ryan M. Holmes, Deepak Cherian, Scott Bachman
Publikováno v:
Journal of Physical Oceanography. 51:1575-1593
The equatorial Pacific cold tongue is a site of large heat absorption by the ocean. This heat uptake is enhanced by a daily cycle of shear turbulence beneath the mixed layer—“deep-cycle turbulence”—that removes heat from the sea surface and d
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::584087239cc1d6948adb5204816a58a1
https://doi.org/10.1175/jpo-d-20-0229.1
https://doi.org/10.1175/jpo-d-20-0229.1
Publikováno v:
Journal of Physical Oceanography. 50:1839-1852
The Lagrangian characteristics of the surface flow field arising when an idealized, anticyclonic, mesoscale, isolated deep-ocean eddy collides with continental slope and shelf topography are explored. In addition to fluid parcel trajectories, we cons
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fc953330a4d0e60eba36637c0d865940
https://doi.org/10.1175/jpo-d-19-0209.1
https://doi.org/10.1175/jpo-d-19-0209.1
Publikováno v:
Journal of Physical Oceanography. 50:323-342
We describe the seasonal cycle of mixing in the top 30–100 m of the Bay of Bengal as observed by moored mixing meters (χpods) deployed along 8°N between 85.5° and 88.5°E in 2014 and 2015. All χpod observations were combined to form seasonal-me
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6d6c400bd649f94051a64ee9e1012ec9
https://doi.org/10.1175/jpo-d-19-0114.1
https://doi.org/10.1175/jpo-d-19-0114.1
Autor:
Joseph Hamman, Anderson Banihirwe, Aureliana Barghini, Alessandro Amici, Stephan Hoyer, Deepak Cherian
A proposal to develop new labelled array data structures for the scientific Python ecosystem
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::9dc8fea4ef27959108f2ef668fb8069e
Autor:
Deepak Cherian, Kenneth H. Brink
Publikováno v:
Journal of Physical Oceanography. 48:1117-1138
Isolated monopolar eddies in the ocean tend to move westward. Those shed by western boundary currents may then interact with the continental margin. This simple picture is complicated by the presence of other flow features, but satellite observations
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9aa712cf55df834602cfd8255483a4f5
https://doi.org/10.1175/jpo-d-17-0237.1
https://doi.org/10.1175/jpo-d-17-0237.1
Autor:
Deepak Cherian, Kenneth H. Brink
Publikováno v:
Journal of Physical Oceanography. 46:3599-3621
At continental margins, energetic deep-ocean eddies can transport shelf water offshore in filaments that wrap around the eddy. One example is that of Gulf Stream warm-core rings interacting with the Mid-Atlantic Bight shelf. The rate at which shelf w
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f2374143804bc859bae0a035b010b362
https://doi.org/10.1175/jpo-d-16-0085.1
https://doi.org/10.1175/jpo-d-16-0085.1
Autor:
Kenneth H. Brink, Deepak Cherian
Publikováno v:
Journal of Marine Research. 71:425-450
Author Posting. © Sears Foundation for Marine Research, 2013. This article is posted here by permission of Sears Foundation for Marine Research for personal use, not for redistribution. The definitive version was published in Journal of Marine Resea
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::83db652022639abe83f569df23c9cddb
https://doi.org/10.1357/002224013812587582
https://doi.org/10.1357/002224013812587582
Autor:
Deepak Cherian, Thomas W. N. Haine
Publikováno v:
Bulletin of the American Meteorological Society. 94:673-684
The dynamics of the rotating shallow-water (RSW) system include geostrophic f low and inertial oscillation. These classes of motion are ubiquitous in the ocean and atmosphere. They are often surprising to people at first because intuition about rotat
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::12267eb3ee26f95e39d4d54ac34ed310
https://doi.org/10.1175/bams-d-12-00023.1
https://doi.org/10.1175/bams-d-12-00023.1