Titlebook: Atmospheric and Oceanic Mesoscale Processes; Maithili Sharan (Professor),Sethu Raman (Professor Book 2007 Birkh?user Basel 2007 Coast.Mons

咽下

執(zhí)拗

Anthropomorphic EMG-Driven Prosthetic Handwest central Bay of Bengal based on observations to up 0300 UTC of the day. A probability of precipitation (PoP) model has been developed by applying forward stepwise regression with available surface and upper air meteorological parameters observed in and around Orissa in association with monsoon d

兒童

George Suciu,Maria-Cristina Di?uugh occur in an overlapping manner under an envelope of low frequency seasonal oscillation. We have also found some correspondence between the summer monsoon rainfall over tropical North Africa and India on a decadal basis, which would suggest a common mode of multi-decadal variability in the two mo

semiskilled

膽大

Anthropomorphic EMG-Driven Prosthetic Handrature, precipitation and snow amount. Model simulations show cold bias over the Himalayan region and warm bias over northwest India. Average monthly distribution of temperature indicates that a controlled experiment could capture the areas of lowest temperature regime. Precipitation fields could be

blithe

Addressing Hurricane Intensity through Angular Momentum and Scale Energetics Approaches The contribution of mean-wave interactions in the kinetic energy varies with distance from the center and with the life stage of a storm. In the early stages, as the disorganized convection becomes organized on the hurricane scales, upscale energy transfers (., from small to large scale) are found

Petechiae

On the Prediction of Tropical Cyclones over the Indian Region Using a Synthetic Vortex Scheme in a M first experiment the model is integrated with a synthetic vortex based on Rankine wind profile while in the second experiment we utilize the Holland wind profile. For the November 2002 cyclone, in both the experiments the model is integrated from 10 November 2002 18 UTC to 12 November, 2002 12 UTC

同位素

虛情假意

無能的人

Observation of Sea Breeze Front and its Induced Convection over Chennai in Southern Peninsular Indiaset is greater in north Chennai. The modal length of sea breeze is between 20 and 50 km with extreme length as high as 100 km also having been observed. Though the inland penetration is on average 10 to 20 km, penetration reaching 100 km was also observed on a number of cases. The induced convection