Zobrazeno 1 - 7
of 7
pro vyhledávání: '"Neeraja C. Reddy"'
Publikováno v:
Pure and Applied Geophysics. 152:781-809
The influence of soil moisture and vegetation variation on simulation of monsoon circulation and rainfall is investigated. For this purpose a simple land surface parameterization scheme is incorporated in a three-dimensional regional high resolution
Publikováno v:
Boundary-Layer Meteorology. 86:125-145
During the Intensive Observation Period (IOP) 7 (22 February 1986) of the Genesis of Atlantic Lows Experiment a persistent coastal front was observed along the Carolina coast in the eastern United States. An intensive baroclinic zone, associated with
Autor:
Neeraja C. Reddy, Sethu Raman
Publikováno v:
Pure and Applied Geophysics PAGEOPH. 147:789-819
A three-dimensional mesoscale numerical model is used to investigate mesoscale circulation over a Gulf Stream filament. Two numerical experiments are performed with different initial uniform ambient wind speeds (U=0.1 m s−1, 3.5 m s−1 and 7 m s
Autor:
M.P. Singh, Sethu Raman, Suman Rao, S. Nigam, P. Agarwal, Amita Gulati, Anil Kumar Yadav, Neeraja C. Reddy
Publikováno v:
Atmospheric Environment. 29:2089-2098
The atmospheric diffusion in the tropics is generally associated with low wind speeds, typically of magnitudes less than 3 ms−1. Low wind speeds would cause significant free convection in the daytime and strong stable conditions in the nighttime. H
Autor:
Neeraja C. Reddy, Sethu Raman
Publikováno v:
Atmospheric Environment. 29:2177-2189
Sensitivity of monsoon rainfall to different ambient wind speeds, orography and wind shear was studied using a two-dimensional mesoscale model. Three numerical experiments were performed with different initial uniform ambient wind speeds (U = 0.1 ms
Autor:
Neeraja C. Reddy, Sethu Raman
Publikováno v:
Boundary-Layer Meteorology. 68:387-417
Turbulence structure of the marine boundary layer (MBL) over the Gulf Stream and the adjacent coastal waters during the development of a storm is discussed. Prestorm conditions prevailed on 9 February and a meso-low formed on 10 February which intens
Autor:
Sethu Raman, Neeraja C. Reddy
Publikováno v:
Tellus A; Vol 48, No 3 (1996)
Observations obtained from aircraft, buoys, ships and vertical soundings made on 9, 10 and 22 February, 1986 during the Genesis of Atlantic Lows Experiment (GALE) are used to study the mean marine boundary-layer (MBL) structure over the cold coastal