Dynamics of the west african monsoon jump
WebDec 23, 2011 · The simulation of the onset of the West African monsoon (WAM), associated with the northward shift of the Intertropical Convergence Zone (ITCZ) occurring in May, June, and July, is a challenging task for atmospheric general circulation models (AGCMs), because of complex water and energy balance through the land-atmosphere … WebJan 10, 2006 · The regional climate model (MAR) is used to perform a simulation of the year 1992 over West Africa. It is shown that MAR is able to simulate the main features of the rainy regime over West Africa and especially the discontinuous seasonal progression of the West African Monsoon along the year. One particular feature that is reasonably well …
Dynamics of the west african monsoon jump
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WebThe West African monsoon jump has been investigated in a number of studies, with several competing ... Hagos and Cook [2007] studied the dynamics of the West African monsoon jump in regional climate model simulations. They analyzed the atmospheric moisture budget and thermodynamics to relate the precipitation
WebWeak monsoon rains produced drought and famine over large parts of Africa in the 1970s and 1980s, but the West African monsoon rains have recovered somewhat since then. So there is evidence that monsoons are changing, but researchers are still investigating how the amount of monsoon rainfall will be affected by climate change in the future. WebJul 15, 2010 · Abstract This study is the last in a series of papers addressing the dynamics of the West African summer monsoon at intraseasonal time scales between 10 and 90 days. The signals of convectively coupled equatorial Rossby (ER) waves within the summer African monsoon have been investigated after filtering NOAA outgoing …
WebGISS) in simulating and predicting the seasonal mean [30] Future works should investigate several questions: and interannual variability of the West African monsoon First, these … WebNov 2, 2024 · The West African Monsoon (WAM) involves the interaction of multi-scale processes ranging from planetary to cumulus scales, which makes it challenging for coarse resolution General Circulation Models to accurately simulate WAM. The present study evaluates the ability of the high-resolution ( $$\\sim$$ ∼ 25 km) Atmospheric General …
WebWest African monsoon jump, regional climate model, absolute vorticity, boundary-layer entropy Abstract The observed seasonal migration of rainfall associated with the West African monsoon (WAM) is characterized by two regimes of relatively intense rainfall: an early, intense peak over the Guinean Coast during late May to early July; and a late ...
WebWest African monsoon progression inland is characterized by a 'jump' between a first regime of high rainfall along the Guinean coast in May to July and a second period of less-intense... soliane landry remaxWebadshelp[at]cfa.harvard.edu The ADS is operated by the Smithsonian Astrophysical Observatory under NASA Cooperative Agreement NNX16AC86A solian buvableWebdemonstrate that West African monsoons and therefore rainfall distribution depend critically on the location of the vegetation perturbations. Changes in vegetation cover along the border between the Sahara desert and West Africa (desertification) may have a minor impact on the simulated monsoon circulation. However, coastal de- solian forumWebDec 27, 1999 · The West African monsoon jump is a sudden change in the position of the rainfall maximum over the continent in boreal summer. Through the spring, the precipitation maximum lies over the... soli and greenWebJun 8, 2006 · The monsoon jump occurs in the unique large-scale dynamics of the West African summer, and the RCM is able to capture that environment accurately. For … smaht definitionWebAs dry/wet spells, etc. Rainfall over West Africa during the name implies, weather regimes affect local weather. the summer monsoon is mainly associated with meso- The “episodic” approach to circulation variability, via scale convective systems, especially over the Sahel cluster analysis, has been shown to be complementary (D’Amato and ... smahtecWebDec 1, 2010 · The WAWJ extends westward to 22°W and strengthens, with a zonal wind maximum of 4 m s −1 at 8°–10°N. Over land, the zonal wind at 14°–18°N is also stronger than in stage 1 as the monsoon flow expands northward to about 19°N over West Africa. The jet reaches peak intensity in stage 3 ( Fig. 2c ). so liang would let him go