Zobrazeno 1 - 9
of 9
pro vyhledávání: '"C. R. V. RAMAN"'
Publikováno v:
Weather. 34:252-257
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b7e1683f70d679575a3f82c586f25487
https://doi.org/10.1002/j.1477-8696.1979.tb03446.x
https://doi.org/10.1002/j.1477-8696.1979.tb03446.x
Publikováno v:
Monthly Weather Review. 109:910-915
In earlier papers it was shown that tropospheric vertical wind shear in the layer 850–200 mb decreases appreciably prior to formation of depressions in the Indian summer monsoon area. Further analysis reveals that this decrease in shear stems almos
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8e99c019bb8b494de4b8eb16a1cfaa91
https://doi.org/10.1175/1520-0493(1981)109<0910:twsoaa>2.0.co
https://doi.org/10.1175/1520-0493(1981)109<0910:twsoaa>2.0.co
Autor:
C. R. V. RAMAN
Publikováno v:
MAUSAM. 15:235-238
While mariners have, for long, associated monsoon with winds, description of monsoonal circulations over land has invariably been designed to explain primarily their rainfall effects. A rainfall oriented definition of monsoon bas several limitations.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d04a7301ae8f4fda150f6bc2f25185d1
https://doi.org/10.54302/mausam.v15i2.5536
https://doi.org/10.54302/mausam.v15i2.5536
Publikováno v:
MAUSAM. 23:327-334
Using correlation techniques, an assessment is made of the influence exerted by basic meteorological factors in controlling .the evoporative power of air. Linear regression equations are developed for twenty five stations linking pan evaporation with
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e30e3966b5c7a6e82fe5a5338d882a8f
https://doi.org/10.54302/mausam.v23i3.5284
https://doi.org/10.54302/mausam.v23i3.5284
Autor:
C. R. V. Raman, Y. Ramanathan
Publikováno v:
Nature. 204:31-35
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e86c171f281152383300ac8fcf67a053
https://doi.org/10.1038/204031a0
https://doi.org/10.1038/204031a0
Publikováno v:
MAUSAM. 22:551-558
Evaporation observations recorded with wire-mesh covered Class A pans at about 80 stations in India for, a period of five years or more have been used to present monthly and annual evaporations maps. Highest evaporation values of 16-17 mm per day are
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9096d4cd6e492684062c6d8d00016856
https://doi.org/10.54302/mausam.v22i4.4989
https://doi.org/10.54302/mausam.v22i4.4989
Autor:
C. R. V. Raman, Jose Maliekal
Publikováno v:
Nature. 314:430-432
Analysis of the causes of the Indian monsoon have concentrated on climatological phenomena in the southern hemisphere, such as El Nino and the Southern Oscillation. By contrast, we have examined meteorological records for the northern hemisphere (0°
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::038534fe27dc14508f2be40cb064d301
https://doi.org/10.1038/314430a0
https://doi.org/10.1038/314430a0
Publikováno v:
Nature. 276:51-53
DEPRESSIONS of the Bay of Bengal are an important component of the south-west monsoon circulation. Moving WNW, they account for much of the rainfall in India. Synoptic conditions favouring formation of monsoon depressions, so far described, are: (1)
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8067c51eb54d86002badc83126755fc2
https://doi.org/10.1038/276051a0
https://doi.org/10.1038/276051a0
Autor:
C. R. V. Raman, Y. P. Rao
Publikováno v:
Nature. 289:271-273
Severe summer droughts of the Indian subcontinent have been found to accompany prolonged ‘breaks’ in the south-west monsoon. Data from the years of severe drought suggest that the associated breaks were due to upper tropospheric blocking ridges o
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e2673224fa72e789cb370297e193dbad
https://doi.org/10.1038/289271a0
https://doi.org/10.1038/289271a0