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• W1574197233 abstract "[1] Coupling recent observed declines of terrestrial mid-latitude near-surface wind speed (u) with knowledge that high-elevation sites rapidly experience climate change led to an assessment of the regional near-surface elevation dependence of u (uZ) at two mountainous regions (central China and Switzerland). The monthly uZ were calculated from 1960–2006. In both regions uZ were higher in winter (∼2.25 m s−1 km−1) compared to summer (∼1.25 m s−1 km−1). For the first time uZ trends were calculated, the results were strongly seasonal, ranging from ∼−0.025 m s−1 km−1 a−1 in winter to ∼−0.005 m s−1 km−1 a−1 in summer. For both regions uZ trend results showed that u has declined more rapidly at higher than lower elevations, even though different u dynamics were observed. The uZ trends have important implications for climatic changes of coupled land-surface/boundary-layer processes (such as evapotranspiration) at high-elevation regions where much of the globe's fresh water is derived." @default.
• W1574197233 created "2016-06-24" @default.
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• W1574197233 date "2010-03-01" @default.
• W1574197233 modified "2023-10-11" @default.
• W1574197233 title "Observational evidence from two mountainous regions that near-surface wind speeds are declining more rapidly at higher elevations than lower elevations: 1960-2006" @default.
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• W1574197233 doi "https://doi.org/10.1029/2009gl042255" @default.
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