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003			ZW-GwMSU
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040			_aMSU _cMSU _erda
100			_aYANG, Yong
245			_aMeasurement and estimation of the summertime daily evapotranspiration on alpine meadow in the Qilian Mountains, northwest China
264			_aVerlag _bSpringer _c2013
336			_2rdacontent _atext _btxt
337			_2rdamedia _aunmediated _bn
338			_2rdacarrier _avolume _bnc
440			_aEnvironmental earth sciences _vVolume , number ,
520			_aResearch on mountain evapotranspiration (ET) is important to help understand water cycling and predict streamflow in cold regions in China. Actual daily ET was measured in two types of micro-lysimeters with depth 40 cm and diameter 31.5 cm (A) and depth 27 cm and diameter 27 cm (B), from 1 July 2007 to 10 September 2007, on an alpine meadow in the Qilian Mountains in northwest China, where Bowen ratio measuring instrument and eddy covariance system are too costly and difficult to be built in the region. The results of micro-lysimeters were used as a way to calibrate and test a number of energy balance methods and determine the pan coefficient (K p) for a mountainous site. The results indicate that the FAO-56 Penman–Monteith offers the best performance, with RMSE of 0.61 mm day−1, MAD of 0.46 mm day−1, and the index of agreement near 1, followed by ASCE Penman–Monteith, Priestley–Taylor and Hargreaves–Samani, and the K p is estimated as 0.7 for the summertime.
650			_aevapotransipiration
650			_amicro-lysimeter
650			_apenman-monteith
700			_aCHEN, Rensheng
700			_aHAN, Chuntan
700			_aQING, Wenwu
856			_uhttps://doi.org/10.1007/s12665-012-1907-5
942			_2lcc _cJA
999			_c161607 _d161607