During the summer monsoon season,the authors observe a wave train that stretches from the northern Arabian Peninsula and Caspian Sea to the Indo-Gangetic plains along the foothills of the Himalaya and extending furthe...During the summer monsoon season,the authors observe a wave train that stretches from the northern Arabian Peninsula and Caspian Sea to the Indo-Gangetic plains along the foothills of the Himalaya and extending further east of the Tibetan Plateau.The trend analysis between 1979 and 2018 with NCEP–NCAR reanalysis data show that the diabatic heating flux(averaged over 1000 to 500 hPa)tends to decrease significantly over the Caspian Sea and its surrounding regions.In addition,the sea level pressure is increasing by^0.1 hPa yr-1 over the Caspian Sea,forming a high-pressure divergent center over there.The divergent center is collocated with an anticyclonic circulation trend at 850 hPa over the Caspian Sea.This decreasing diabatic heating flux modulates the local atmospheric circulation by increasing the surface pressure around the center of divergence,which further facilitates a wave train to propagate towards South and East Asia.This wave train transports the moisture fluxes at 925 h Pa from the Caspian Sea,southeastward towards the South and East Asian monsoon region.展开更多
The Taklamakan Desert in China is one of the major source regions for Asian dust particles.All balloon-borne measurements in this report were carried out in Dunhuang,in the Taklamakan Desert,during calm weather condit...The Taklamakan Desert in China is one of the major source regions for Asian dust particles.All balloon-borne measurements in this report were carried out in Dunhuang,in the Taklamakan Desert,during calm weather conditions.The aerosol number concentration,size distribution,mass concentration,and horizontal mass flux due to westerly wind were investigated.The measurements were performed on 17 August 2001,17 October 2001,11 January 2002,and 30 April 2002.Five channels(0.3,0.5,0.8,1.2,and 3.6μm in diameter)were used in the Optical Particle Counter for particle measurements.The aerosol number concentration in the winter season(11 January 2002)at 3–5 km was very high.Variation of free-tropospheric aerosols on 30 April 2002 was noticeable.A super-micron range was noticeable in the size distribution of all the measurements.Many variations in temperature and aerosol concentration were found at these inversion points.High values of estimated mass concentration of aerosols were frequently observed in the atmosphere near the ground(i.e.,1–2 km);and interestingly,relatively high concentrations were frequently detected above 2 km from the surface.Wind patterns observed using ERA-Interim data at 500 and 850 hPa showed that westerly winds dominated in the Taklamakan Desert during the observation period.The average horizontal mass flux of background Asian dust due to westerly wind was observed to fall within the range of 58.5–1219 tons km?2 d?1.Vertical profiles of aerosol number concentrations showed that significant transport of aerosols dominated in the westerly region(i.e.,4–7 km).展开更多
基金supported by the Ministry of Science and Technology of China grant number 2016YFA0600604the National Natural Science Foundation of China grant numbers 41950410756 and 41675061the Key Research Program of Frontier Sciences,Chinese Academy of Sciences grant number QYZDY-SSW-DQC024。
文摘During the summer monsoon season,the authors observe a wave train that stretches from the northern Arabian Peninsula and Caspian Sea to the Indo-Gangetic plains along the foothills of the Himalaya and extending further east of the Tibetan Plateau.The trend analysis between 1979 and 2018 with NCEP–NCAR reanalysis data show that the diabatic heating flux(averaged over 1000 to 500 hPa)tends to decrease significantly over the Caspian Sea and its surrounding regions.In addition,the sea level pressure is increasing by^0.1 hPa yr-1 over the Caspian Sea,forming a high-pressure divergent center over there.The divergent center is collocated with an anticyclonic circulation trend at 850 hPa over the Caspian Sea.This decreasing diabatic heating flux modulates the local atmospheric circulation by increasing the surface pressure around the center of divergence,which further facilitates a wave train to propagate towards South and East Asia.This wave train transports the moisture fluxes at 925 h Pa from the Caspian Sea,southeastward towards the South and East Asian monsoon region.
基金supported by the National Natural Science Foundations of China [grant numbers 41590871 and 41475136]the International Science&Technology Cooperation Program of China [grant number 2013DFG22820]
文摘The Taklamakan Desert in China is one of the major source regions for Asian dust particles.All balloon-borne measurements in this report were carried out in Dunhuang,in the Taklamakan Desert,during calm weather conditions.The aerosol number concentration,size distribution,mass concentration,and horizontal mass flux due to westerly wind were investigated.The measurements were performed on 17 August 2001,17 October 2001,11 January 2002,and 30 April 2002.Five channels(0.3,0.5,0.8,1.2,and 3.6μm in diameter)were used in the Optical Particle Counter for particle measurements.The aerosol number concentration in the winter season(11 January 2002)at 3–5 km was very high.Variation of free-tropospheric aerosols on 30 April 2002 was noticeable.A super-micron range was noticeable in the size distribution of all the measurements.Many variations in temperature and aerosol concentration were found at these inversion points.High values of estimated mass concentration of aerosols were frequently observed in the atmosphere near the ground(i.e.,1–2 km);and interestingly,relatively high concentrations were frequently detected above 2 km from the surface.Wind patterns observed using ERA-Interim data at 500 and 850 hPa showed that westerly winds dominated in the Taklamakan Desert during the observation period.The average horizontal mass flux of background Asian dust due to westerly wind was observed to fall within the range of 58.5–1219 tons km?2 d?1.Vertical profiles of aerosol number concentrations showed that significant transport of aerosols dominated in the westerly region(i.e.,4–7 km).
