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

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樓主: Monsoon
41#
發(fā)表于 2025-3-28 17:08:51 | 只看該作者
Variability of Convective Activity over the North Indian Ocean and its Associations with Monsoon Rai-ii; 1992 to 2004) compared to that of the former period (period -i; 1979 to 1991) during JJAS and is associated with a significantly increasing trend (at 95% level) of convective activity over the north Bay of Bengal (NBAY). On a monthly scale, July and August also show increase in convective activ
42#
發(fā)表于 2025-3-28 21:19:36 | 只看該作者
The Assimilation of GPS Radio Occultation Data and its Impact on Rainfall Prediction along the West n good agreement with rainfall observations, up to 72-h forecast. There are some subtle but important differences in predicted rainfalls between the control run CN (without the assimilation of refractivity soundings) and G13 (with the assimilation of thirteen GPS RO soundings). In general, the assim
43#
發(fā)表于 2025-3-29 02:04:47 | 只看該作者
Sensitivity of Mesoscale Model Forecast During a Satellite Launch to Different Cumulus Parameterizatod 25th April to 04th May, 2005 over the Indian region and surrounding oceans were made using different CPSs. The 24 h and 48 h model predicted wind, temperature and moisture fields for different CPSs, namely the Kuo, Grell, Kain-Fritsch and Betts-Miller, are statistically evaluated by calculating p
44#
發(fā)表于 2025-3-29 03:12:31 | 只看該作者
Experimental Seasonal Forecast of Monsoon 2005 Using T170L42 AGCM on PARAM Padma Mission (TRMM) estimates for the 2005 monsoon season. Compared to the model climatology (7.81 mm/day), the model had simulated a normal rainfall (7.75 mm/day) for the year 2005 which is in agreement with the observations (99% of long-term mean). However, the model could not capture the observed inc
45#
發(fā)表于 2025-3-29 10:55:52 | 只看該作者
An Objective Approach for Prediction of Daily Summer Monsoon Rainfall over Orissa (India) due to Intwest 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
46#
發(fā)表于 2025-3-29 14:00:54 | 只看該作者
Interactive Aspects of the Indian and the African Summer Monsoon Systemsugh 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
47#
發(fā)表于 2025-3-29 18:16:48 | 只看該作者
The Preferred Structure of the Interannual Indian Monsoon Variability the India Meteorological Department (IMD) between strong years and normal years (weak years and normal years) are statistically significant over central India, with strong (weak) years associated with increased (decreased) precipitation. In both cases the maps of rainfall anomalies are of one sign
48#
發(fā)表于 2025-3-29 21:59:39 | 只看該作者
Wintertime Seasonal Scale Simulation over Western Himalaya Using RegCM3rature, 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
49#
發(fā)表于 2025-3-30 03:42:00 | 只看該作者
Marko Peri?a,Petra Zori?,Valentina Ani?ulus parameterization schemes of Ferrier . and Betts-Miller-Janjic was able to capture the heavy rainfall events better than the other schemes. It is also observed that the WRF model was able to predict mesoscale rainfall more realistically in comparison to the Eta model of the same resolution.
50#
發(fā)表于 2025-3-30 07:38:49 | 只看該作者
Sheri Osborn,Kim-Kwang Raymond Choorainfall are sensitive to the formulation of entrainment and detrainment in a mass flux scheme, and that the new formulation can effectively represent the increased dilution with height in deep clouds.
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