2014
DOI: 10.1007/s10546-014-9971-x
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Characteristics of Dew Formation and Distribution, and Its Contribution to the Surface Water Budget in a Semi-arid Region in China

Abstract: Observations in the semi-arid Loess Plateau area of north-west China are utilized to reveal the characteristics and variations in the seasonal distribution of dewfall (frost) and the influence of micrometeorology, precipitation, and other weather conditions. Precipitation is the dominant water source in the Loess Plateau; however, non-rainfall water accounts for 13 % of the total land-surface water source. Dew is the second largest non-rainfall component next only to soil adsorption water. Observations show th… Show more

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Cited by 57 publications
(48 citation statements)
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“…According to Monteith (1957), dew would not condense once wind speed (at 2-m height) will be below 0.5 m s −1 , that is, below the necessary threshold which guarantees efficient heat exchange with air and a constant supply of vapour. Although some reported lower thresholds for the high wind speed (1.9 m s −1 see Zhang et al, 2015, or 2.4 m s −1 see Long, 1958), most researchers found a similar threshold of 5 m s −1 . Subsequent measurements generally agree with these thresholds.…”
Section: Figurementioning
confidence: 98%
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“…According to Monteith (1957), dew would not condense once wind speed (at 2-m height) will be below 0.5 m s −1 , that is, below the necessary threshold which guarantees efficient heat exchange with air and a constant supply of vapour. Although some reported lower thresholds for the high wind speed (1.9 m s −1 see Zhang et al, 2015, or 2.4 m s −1 see Long, 1958), most researchers found a similar threshold of 5 m s −1 . Subsequent measurements generally agree with these thresholds.…”
Section: Figurementioning
confidence: 98%
“…Subsequently, whereas Kidron et al (2002a) concluded that dew may only serve as a marginal water source for biocrusts, other researchers maintained that NRW may play an important role in the water balance of biocrusts. Based on ML measurements, dew was reported to take place already at RH values as low as 80-86% (Uclés et al, 2015;Zhang et al, 2015). Figure 3 presents the different factors that affect NRW.…”
Section: Distribution Amount and Durationmentioning
confidence: 99%
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“…During the growing season, the Le was higher than the He within a certain morning time interval from April to August (Figure 2) because evaporation of condensation resulted in high Le [47][48][49], whereas the He increased significantly relative to the Le at noon due to strong turbulence. The Le showed a small transient decrease before the daytime maximum Le was reached, which may be attributable to the presence of local mountain-valley winds ( Figure 6 and Table 2).…”
Section: Land-atmosphere Heat Exchangementioning
confidence: 99%