Zobrazeno 1 - 7
of 7
pro vyhledávání: '"Vijayakumar Manghnani"'
Autor:
Devdutta S. Niyogi, John M. Morrison, Sethu Raman, Vijayakumar Manghnani, J. V. S. S. Raju, Vinayaka Parameswara, S. V. Ramana
Publikováno v:
Boundary-Layer Meteorology. 97:411-430
The variability in boundary-layer structure over the Indian Ocean during a north-east monsoon and the factors influencing it are investigated. This study was made possible as a component of the Indian Ocean Experiment (INDOEX), conducted from Februar
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d9e662edf8bcb476305931b9f65c965b
https://doi.org/10.1023/a:1002730405170
https://doi.org/10.1023/a:1002730405170
Publikováno v:
Deep Sea Research Part II: Topical Studies in Oceanography. 47:1227-1247
Satellite-derived sea-surface temperature, TOPEX/POSEIDON (T/P) sea-level anomalies (SLAs), model wind data, and hydrographic data are used to characterize the upwelling along the Oman coast during the US Joint Global Ocean Flux Study (US JGOFS) Arab
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ef9b0a0102c6d06e018b2eb462e83a67
https://doi.org/10.1016/s0967-0645(99)00142-3
https://doi.org/10.1016/s0967-0645(99)00142-3
The Ras al Hadd Jet: Remotely sensed and acoustic Doppler current profiler observations in 1994–1995
Publikováno v:
Deep Sea Research Part II: Topical Studies in Oceanography. 46:1531-1549
The existence of a surface barotropic front-jet system at the confluence region off the eastern tip of Oman (Ras Al Hadd or RAH) is documented for 1994–1995 through advanced very high resolution radiometer (AVHRR) and acoustic Doppler current profi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1f4fed0e1fc4429b17e5dd059443197f
https://doi.org/10.1016/s0967-0645(99)00034-x
https://doi.org/10.1016/s0967-0645(99)00034-x
Publikováno v:
Deep Sea Research Part II: Topical Studies in Oceanography. 46:1551-1575
TOPEX/POSEIDON altimeter data and wind data are used to calculate the geostrophic transport and Ekman transport in the northern Arabian Sea within the upper 500 m. In the summer, the upper 500-m layer in the northern Arabian Sea is horizontally diver
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::02f66232be9de5450aa156fc62590595
https://doi.org/10.1016/s0967-0645(99)00035-1
https://doi.org/10.1016/s0967-0645(99)00035-1
Autor:
Jan S. Gundersen, Vijayakumar Manghnani, Karen F. Wishner, S. W. A. Naqvi, John M. Morrison, L.A Codispoti, Charles N. Flagg, Linda Prosperie, Steve Gaurin, Sharon L. Smith, Wilford D. Gardner
Publikováno v:
Deep Sea Research Part II: Topical Studies in Oceanography. 46:1903-1931
This paper focuses on the characteristics of the oxygen minimum zone (OMZ) as observed in the Arabian Sea over the complete monsoon cycle of 1995. Dissolved oxygen, nitrite, nitrate and density values are used to delineate the OMZ, as well as identif
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e6a9191a5aeaadcc7bda2f1f08f975f9
https://doi.org/10.1016/s0967-0645(99)00048-x
https://doi.org/10.1016/s0967-0645(99)00048-x
Seasonal variation of hydrographic and nutrient fields during the US JGOFS Arabian Sea Process Study
Publikováno v:
Deep Sea Research Part II: Topical Studies in Oceanography. 45:2053-2101
Between September 1994 and December 1995, the US JGOFS Arabian Sea Process Experiment collected extensive, high quality hydrographic data (temperature, salinity, dissolved oxygen and nutrients) during all seasons in the northern Arabian Sea. An analy
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f8d4b49486ee7be0a6a28c7b42dbee7f
https://doi.org/10.1016/s0967-0645(98)00063-0
https://doi.org/10.1016/s0967-0645(98)00063-0
Publikováno v:
Deep Sea Research Part II: Topical Studies in Oceanography. 45:2027-2052
Advanced Very High Resolution Radiometer (AVHRR) imagery of sea-surface-temperature, TOPEX/POSEIDON measurements of sea-level-anomaly (SLA), and modeled surface winds and wind-stress fields are used in concert with other ancillary data to describe th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::835c5015a9bb36916bdf4fc67c3dadf9
https://doi.org/10.1016/s0967-0645(98)00062-9
https://doi.org/10.1016/s0967-0645(98)00062-9