The spatial pattern of summertime subtropical anticyclones over Asia and Africa: A climatological review

• Published in: International Journal of Climatology
• Main Authors: Zarrin, Azar, Ghaemi, Hooshang, Azadi, Majid, Farajzadeh, Manuchehr
• Format: Article in Journal/Newspaper
• Language: English
• Published: Wiley 2009
• Subjects: North Atlantic
• Online Access: http://dx.doi.org/10.1002/joc.1879; https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fjoc.1879; https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/joc.1879

Abstract The National Centers for Environmental Prediction‐National Center for Atmospheric Research (NCEP‐NCAR) monthly mean reanalysis dataset has been used to analyze spatial variations of summertime subtropical anticyclones over the Asia–Africa region. The geopotential height and zonal wind components of 1000, 500, 200, and 100 hPa in a 30‐year period (1971–2000) have been used to determine the spatial and temporal variations of the anticyclone centres, their monthly frequency and latitudinal axis variations during April–October. The results revealed that there is a clear difference in the location of the summer anticyclone centres in lower, middle and upper levels of the troposphere. In the lower levels, the Azores subtropical anticyclone is located at the east of North Atlantic. In the middle levels, the frequencies of anticyclone centre are concentrated over the northwest of Africa, Arabian Peninsula and Iranian Plateau. In the upper troposphere, the geographical location of the anticyclone centres and their frequencies in the summer season exhibit a scattered pattern from south of China up to western Iran at 200 hPa, and a bimodal pattern over the Tibetan and the Iranian Plateaus at 100 hPa. In fact, in the entire study domain, the Iranian Plateau is a preferable location of the middle and upper troposphere anticyclones. The highest observed latitude of the subtropical anticyclone at 100, 200 and 500 hPa levels have been seen over north of Tibetan plateau, a large area from east to west of Asia and Iran during August, July–August and July, respectively. The maximum monthly variation in the latitude of the ridgeline is seen at 500, 200, and 100 hPa from June to July which goes even up to 10 degrees at some longitudes. Copyright © 2009 Royal Meteorological Society