2018
DOI: 10.5846/stxb201704070595
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Effects of biological soil crusts on the characteristics of hygroscopic and condensate water deposition in alpine sandy lands

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Cited by 2 publications
(2 citation statements)
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“…The percentage of annual condensation water to annual precipitation was in the order of Gonghe > Xinghai > Yushu > Maqin > Zeku > Banma. The variation trend of condensation water, the range of daily condensation water, and the annual amount of condensation water were consistent with the research results of the Fenghuoshan Basin [35], Heihe Basin [36], and Shazhuyu alpine sandy areas [37]. The amount of condensation water during the year showed a bimodal trend (see Figure 4), with the lowest amounts in winter and spring, the largest in late summer and early autumn (August), and the second-largest in late autumn and early winter (October and November).…”
Section: Analysis Of Condensation Water Of Different Vegetationsupporting
confidence: 88%
“…The percentage of annual condensation water to annual precipitation was in the order of Gonghe > Xinghai > Yushu > Maqin > Zeku > Banma. The variation trend of condensation water, the range of daily condensation water, and the annual amount of condensation water were consistent with the research results of the Fenghuoshan Basin [35], Heihe Basin [36], and Shazhuyu alpine sandy areas [37]. The amount of condensation water during the year showed a bimodal trend (see Figure 4), with the lowest amounts in winter and spring, the largest in late summer and early autumn (August), and the second-largest in late autumn and early winter (October and November).…”
Section: Analysis Of Condensation Water Of Different Vegetationsupporting
confidence: 88%
“…Researchers in China have investigated surface condensation water in different regions. Bin et al [10] studied the formation characteristics of condensation water in the Maowusu Sand and its influence on water balance; Xiaohan et al [11] investigated the characteristics of surface condensation water under different types of sand-fixing shrubs in the Maousu Sandy Area; Zhifeng et al [12] investigated the source of water vapor in soil condensation in the Guanzhong Plain; Wanpeng et al [13] investigated the formation characteristics of soil condensate in Cocosi; Qiancheng et al [14] investigated the characteristics of soil condensation and the source of water vapor in winter deserts; Chunjie et al [15] explored the evaporative condensation in the Qinghai-Tibet Plateau region; Long et al [16] investigated the effect of biological soil crust on condensation in alpine sand areas; Rongyi et al [17] analyzed the formation of soil condensation in the Gurbantunggut Desert; Yanxia et al [18] discussed the influence of topography on condensation in the Shapotou area; and Bin et al [19] studied soil condensation in different substrates of the Tarim River.…”
Section: Introductionmentioning
confidence: 99%