气候与环境研究
氣候與環境研究
기후여배경연구
CLIMATIC AND ENVIRONMENTAL RESEARCH
2009年
4期
352-362
,共11页
半干旱%陆面过程模式%能量通量
半榦旱%陸麵過程模式%能量通量
반간한%륙면과정모식%능량통량
semi-arid%land surface model%energy flux
随着全球气候变化和伴随而来的日益严重的干旱化问题,干旱/半干旱地区的陆气相互作用引起了越来越多的重视.利用国际协同强化观测期(CEOP)观测资料对3个不同的陆面过程模式BATS、LSM和CoLM在半干旱区通榆站进行了模拟检验与对比,考察了不同陆面过程模式对半干旱地区的模拟性能.结果表明,3个模式都可以较好地模拟出半干旱地区地气间的能量通量的季节和日变化,但模拟性能存在较大差异.对于地表温度和出射长波辐射的模拟,BATS表现最优;而对于感热和潜热通量的模拟,CoLM和LSM要好于BATS,其中CoLM的表现最好.各模式的模拟性能随着季节不同存在着很大的差异,夏季的模拟要好于冬季,3个模式都不能很好地模拟冬季该地区的潜热通量,说明对半干旱地区冬季地表过程的刻画还有待进一步提高.
隨著全毬氣候變化和伴隨而來的日益嚴重的榦旱化問題,榦旱/半榦旱地區的陸氣相互作用引起瞭越來越多的重視.利用國際協同彊化觀測期(CEOP)觀測資料對3箇不同的陸麵過程模式BATS、LSM和CoLM在半榦旱區通榆站進行瞭模擬檢驗與對比,攷察瞭不同陸麵過程模式對半榦旱地區的模擬性能.結果錶明,3箇模式都可以較好地模擬齣半榦旱地區地氣間的能量通量的季節和日變化,但模擬性能存在較大差異.對于地錶溫度和齣射長波輻射的模擬,BATS錶現最優;而對于感熱和潛熱通量的模擬,CoLM和LSM要好于BATS,其中CoLM的錶現最好.各模式的模擬性能隨著季節不同存在著很大的差異,夏季的模擬要好于鼕季,3箇模式都不能很好地模擬鼕季該地區的潛熱通量,說明對半榦旱地區鼕季地錶過程的刻畫還有待進一步提高.
수착전구기후변화화반수이래적일익엄중적간한화문제,간한/반간한지구적륙기상호작용인기료월래월다적중시.이용국제협동강화관측기(CEOP)관측자료대3개불동적륙면과정모식BATS、LSM화CoLM재반간한구통유참진행료모의검험여대비,고찰료불동륙면과정모식대반간한지구적모의성능.결과표명,3개모식도가이교호지모의출반간한지구지기간적능량통량적계절화일변화,단모의성능존재교대차이.대우지표온도화출사장파복사적모의,BATS표현최우;이대우감열화잠열통량적모의,CoLM화LSM요호우BATS,기중CoLM적표현최호.각모식적모의성능수착계절불동존재착흔대적차이,하계적모의요호우동계,3개모식도불능흔호지모의동계해지구적잠열통량,설명대반간한지구동계지표과정적각화환유대진일보제고.
With the global climate change and the aridification in northern China, more and more studies have focused on the land-atmosphere interactions in arid/semi-arid areas. The goal of this presentation is to evaluate land surface models BATS, LSM, and CoLM in semi-arid areas using the Coordinated Enhanced Observing Period (CEOP) data, with an emphasis on comparison of the performance of the three models in semi-arid regions. The results show that all of the three models can simulate the diurnal and seasonal cycle of the fluxes between land surface and atmosphere in this region, but the performance varies largely among them. For the simulations of the ground surface temperature and ground emitted longwave radiation, BATS is better than LSM and CoLM. As to sensible and latent heat flux, CoLM and LSM are better, and CoLM is! The best. The performance of the three models varies with seasons, with summer better than winter. It is significant that all three models can not simulate the latent heat flux well in winter, which indicates that the current LSMs should pay more attention to improve the simulating performance in semi-arid areas in winter.