沙漠与绿洲气象
沙漠與綠洲氣象
사막여록주기상
DESERT AND OASIS METEOROLOGY
2012年
4期
38-43
,共6页
数值模拟%区域气候模式%降水%气温
數值模擬%區域氣候模式%降水%氣溫
수치모의%구역기후모식%강수%기온
simulation%regional climate model%precipitation%air temperature
通过数值模拟方法,研究了降水和气温对模式分辨率、初始和边界条件的敏感性。结果表明:区域模式RegCM3对新疆1996年冬季和夏季的降水和气温具有一定的模拟能力,气温的模拟要优于降水。分辨率、初始和边界条件对区域模式的模拟结果有较大的影响。模式分辨率的提高,可以增强对气温的模拟能力,尤其是气温随地形变化的特点。分辨率的提高,同样可以改进降水的量级和落区。相同分辨率下,不同初始和边界条件,对降水的模拟结果影响不大。无论分辨率和初始,边界条件如何变化,塔克拉玛干沙漠南麓均有虚假降水出现,说明该模式在刻画复杂地形方面,还存在不足。
通過數值模擬方法,研究瞭降水和氣溫對模式分辨率、初始和邊界條件的敏感性。結果錶明:區域模式RegCM3對新疆1996年鼕季和夏季的降水和氣溫具有一定的模擬能力,氣溫的模擬要優于降水。分辨率、初始和邊界條件對區域模式的模擬結果有較大的影響。模式分辨率的提高,可以增彊對氣溫的模擬能力,尤其是氣溫隨地形變化的特點。分辨率的提高,同樣可以改進降水的量級和落區。相同分辨率下,不同初始和邊界條件,對降水的模擬結果影響不大。無論分辨率和初始,邊界條件如何變化,塔剋拉瑪榦沙漠南麓均有虛假降水齣現,說明該模式在刻畫複雜地形方麵,還存在不足。
통과수치모의방법,연구료강수화기온대모식분변솔、초시화변계조건적민감성。결과표명:구역모식RegCM3대신강1996년동계화하계적강수화기온구유일정적모의능력,기온적모의요우우강수。분변솔、초시화변계조건대구역모식적모의결과유교대적영향。모식분변솔적제고,가이증강대기온적모의능력,우기시기온수지형변화적특점。분변솔적제고,동양가이개진강수적량급화락구。상동분변솔하,불동초시화변계조건,대강수적모의결과영향불대。무론분변솔화초시,변계조건여하변화,탑극랍마간사막남록균유허가강수출현,설명해모식재각화복잡지형방면,환존재불족。
The Sensitivities of precipitation and air temperature to several key physical processes, such as resolution, initial and lateral boundary conditions, were studied. The results showed the regional climate model (RegCM3) in some extent could simulate the pattern of precipitation and air temperature in winter and summer in Xinjiang in 1996,and the simulation of air temperature was better than precipitation. The resolution, initial and lateral boundary conditions of model had effects on the simulation results in some extent. With higher resolution,it could improve simulating capacities of air temperature,especially around big terrains. When increasing resolution, the precipitation grade and area also could be improved. Under the same resolution, the initial and lateral boundary conditions of model had no effects on precipitation. In spite of any resolution or initial and lateral boundary conditions,there were false precipitation in southern area of taklimakan desert, which indicated that the model had some deficiencies of depicting complex terrain.