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Weisheng Wang, Meiping Sun, Yanjun Che, Xiaojun Yao, Mingjun Zhang and Shuting Niu
Worldwide, there are great challenges for meteorological monitoring and glacier ablation monitoring in high-altitude mountain areas. It is often difficult to capture fine-scale climate and glacial changes in high-altitude mountainous areas due to the har...
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Juerg Schmidli, Steven Böing and Oliver Fuhrer
We evaluate the near-surface representation of thermally driven winds in the Swiss Alps in a numerical weather prediction model at km-scale resolution. In addition, the influence of grid resolution (2.2 km and 1.1 km), topography filtering, and land surf...
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Stefano Serafin, Bianca Adler, Joan Cuxart, Stephan F. J. De Wekker, Alexander Gohm, Branko Grisogono, Norbert Kalthoff, Daniel J. Kirshbaum, Mathias W. Rotach, Jürg Schmidli, Ivana Stiperski, ?eljko Vecenaj and Dino Zardi
The exchange of heat, momentum, and mass in the atmosphere over mountainous terrain is controlled by synoptic-scale dynamics, thermally driven mesoscale circulations, and turbulence. This article reviews the key challenges relevant to the understanding o...
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Júlia Wahrlich,Flávia Arcari da Silva,Claudia Guimarães Camargo Campos,Maria Laura Guimarães Rodrigues,Jéssica Medeiros
Although the state of Santa Catarina has little variation in latitude, it presents significant spatial variations in its climate. Wind is considered an important meteorological variable, but it is not intensively studied and there is a shortage of inform...
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Mélissa Cholette, René Laprise and Julie Mireille Thériault
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NAND LAL SHARMA,JAGDISH CHANDRA KUNIYAL,RAJ PAUL GULERIA,MAHAVIR SINGH
Observations from a ground based multi-wavelength radiometer (MWR) in the Kullu valley of the North Western Himalayan region from April 2007 to March 2008 show that the spectral aerosol optical depth (AOD) and the Ångstr?m turbidity coefficient (ß) are h...
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ERNESTO JAUREGUI
Components of the thermotopographic wind regime in the Mexico City basin are examined in their interaction with the heat island induced centripetal circulation. The resulting wind regime is such that convergent surface flow over the city is predominan...
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