Pritchard, M. S., M. W. Moncrieff and R. C. J. Somerville, in press (Manuscript received 12 October 2010, in final form 8 February 2011): Orogenic Propagating
Precipitation Systems over the United States in a Global Climate Model with Embedded Explicit Convection.
Not exact matches
«This cooling reduced
precipitation over Africa, and in combination with a range of other complex climate feedback mechanisms tipped the humid
system towards aridification,» explains the first author of the study, James Collins from Helmholtz Centre Potsdam — GFZ German Research Centre for Geosciences and Alfred Wegener Institute — Helmholtz Center for Polar and Marine Research (AWI) in Bremerhaven.
Over the past several years, scientists from many institutions have explored the ability of SP - CAM to simulate tropical weather
systems, the day - night changes of
precipitation, the Asian and African monsoons, cloud - aerosol interactions and other climate phenomena.
Slow - moving weather
systems are another factor in heavy
precipitation, as a slower - moving
system can produce more rain
over particular area.
In 2010, intense
precipitation concentrated
over the elevated plains of Khyber Pakhtunkhwa due to interaction of three weather
systems from east, south and north.
One year (August 1998ï ¿ 1/2 July 1999) of tropical rainfall estimates from the
Precipitation Estimation from Remotely Sensed Information using Artificial Neural Networks (PERSIANN)
system were used to produce monthly means of rainfall diurnal cycles at hourly and 1ï ¿ 1/2 ï ¿ 1/2 1ï ¿ 1/2 scales
over a domain (30ï ¿ 1/2 Sï ¿ 1/2 30ï ¿ 1/2 N, 80ï ¿ 1/2 Eï ¿ 1/2 10ï ¿ 1/2 W) from the Americas across the Pacific Ocean to Australia and eastern Asia.
This process prevents the land — atmosphere
system from sustaining
precipitation over the same region and thus acts against drought or the formation of desert.
A 2013 study modeled climate and water
system (hydroclimate) changes in the Western US
over the next three decades and found that increased temperature is the dominant factor, likely leading to several hydroclimate changes, including: decreases in spring snow pack, increases in cold - season days above freezing, and decreases in the cold - season snow - to -
precipitation ratio.
«Relatively cool waters in the eastern Pacific often result in stubborn summer high - pressure
systems over the eastern states that block storms, reducing the frequency of
precipitation below normal,» noted study co-author Richard Healy of the Woods Hole Oceanographic Institution, Woods Hole, Mass. «Less frequent storms result in higher surface and atmospheric temperatures that then feedback on the atmospheric circulation to further reduce storm frequency and raise surface temperatures even more.»
Monthly temperature,
precipitation, 500hPa geopotential height, mean sea - level pressure and soil moisture
over the entire globe are also output to assess larger scale weather
systems.
We also show that this change is reflected in the tropical cyclone
systems and finally on the
precipitation patterns
over the Indian region as they are interlinked.