Review of Advances in World Dryland Climate Research (Ⅱ):Main Investigation Progress

  • QIAN Zheng'an ,
  • SONG Minhong ,
  • WU Tongwen ,
  • CAI Ying
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  • Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, Gansu, China;Chengdu University of Information Technology, Chengdu 610225, Sichuan, China;National Climate Center, China Meteorological Administration, Beijing 100081, China

Received date: 2017-04-24

  Online published: 2017-12-28

Abstract

As the continued paper of the review (Ⅰ), the paper (Ⅱ) will further review the main progresses in world dryland climate, including drought indices, arid-and semiarid-zone dividing and their distribution, dryland climate changes, forming causes and projecting. The main points are as follows:(1) More than dozens availability drought "indices" have already put out in various countries, they are well-used in home and abroad. Say, the PDSI, SPI and NDVI indices and so on in the US. (2) Nowdays more researchers utilize the "moisture availability as the "criteria" in dividing the dry areas. Among nearly 10 existed arid-and semiarid-zone maps have been published, the map of Hulme and Marsh is more closer to the real world. On the average, the arid-and semiarid-area make totally up 35% of the global land area, they cover the 8 major arid areas:ie, the North Africa, Australia and China-Mongolia ones and so on; there are the home of about 20 billion people of the globe. (3) The global climate changes in past 1 000 (especially in the recent 100) years are mainly characterized by global warming of the surface air temperature and the larger temporal-and spatial-changes of precipitation climate. Due to the increased CO2 and CH4 greenhouse gasses, the global mean temperature increased 0.56~0.92℃ in the past 100 years. In contrast, beyond the East Asia and North Africa, the precipitation climate change links among other dry zones are not so close to each other. There are two combination partterns for temperature and precipitation change in various dry zone in the past. (4) There are many ways for the drought causes across the world arid zones. From the recent discussions about North Africa and China-Mongolia drought causes, it is seemely that the global arid climate forming may classified briefly in two types only:namely global tropical warm SST and mountain topography impact ones. North Africa and China-Mongolia arid areas are the respectively representation of the two types. The discussions show:for the former, it is caused by mainly the global warm SST, especially in the tropical zone and secondly by the land-air interaction; for the latter, by mainly the Qinghai-Xizang Plateau topography and secondly by the circulation. (5) The key point of the arid climate prediction is the one of the decodal drought. There are long road to go for the arid climate prediction.

Cite this article

QIAN Zheng'an , SONG Minhong , WU Tongwen , CAI Ying . Review of Advances in World Dryland Climate Research (Ⅱ):Main Investigation Progress[J]. Plateau Meteorology, 2017 , 36(6) : 1457 -1476 . DOI: 10.7522/j.issn.1000-0534.2017.00076

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