Effects of variability in landscape types on the microclimate across a desert–oasis region on the southern margins of the Tarim Basin, China. Issue 1 (2nd January 2016)

• Record Type: Journal Article
• Authors: Mao, Donglei; Lei, Jiaqiang; Zhao, Ying; Zhao, Jianping; Zeng, Fanjiang; Xue, Jie
• Is Part Of: Arid land research and management. Volume 30:Issue 1(2016)
• Page Start: 89
• Page End: 104
• Publication Date: 2016-01-02
• Subjects: Cele -- desert–oasis ecotone -- microclimate -- oasis -- spatial variation; Arid soils -- Periodicals; Arid regions agriculture -- Periodicals; Desert reclamation -- Periodicals; 631.47154
• DOI: 10.1080/15324982.2015.1055851
• Languages: English
• ISSNs: 1532-4982

Abstract

ABSTRACT: Microclimates play important roles in controlling water budgets and water vapor transportation, as well as vegetation growth characteristics. In order to understand the differences in meteorological parameters under different vegetation cover (VC) and terrain conditions, wind velocity, air temperature, relative humidity (RH), photosynthetically active radiation (PAR), and solar radiation were simultaneously monitored on shifting, semi-fixed and fixed sandy lands, and an oasis. The air temperature and RH differences among the four landscape types were obvious in the period from May to October. It was found that the higher elevations of semi-fixed sandy land can influence PAR and solar radiation during sand-blowing weather. The differences of air temperature and RH among the four sites during the dust-storm and rainy days were not obvious, but their differences during sand-blowing weather were greater than during rainy weather and less than during floating-dust and sunny weather. The differences of PAR and solar radiation among the four landscape types were most obvious during the dust-storm event. During most of the weather types studied, significant positive correlations were found between wind velocity and temperature, PAR, and solar radiation, as well as between temperature and PAR, and solar radiation. Meanwhile, significant negative correlations were found between RH and wind velocity, temperature, PAR, and solar radiation. VC and topography were found to be the main factors influencing the changes in meteorological parameters between desert–oasis ecotone and oasis.