摘要
根据已初步建立的零维地表能量平衡模式,利用考察资料及邻近气象站资料,对大别山南段赵公岭山区3.0×3.5km^2区域进行计算(网格距为100m),首次绘制出该山区1、7月平均气温分布图。结果表明:冬季,山区温度场分布在很大程度上决定于地形条件;夏季,地形的影响要小的多。
This study is the subsequent work on the numerical simulation of radiationand heat balance over the hilly land. Based on the zero-dimensional surface heat balancemodel proposed in the previous article,into which are fed the data from investigation andthe weather stations in the vicinity, calculation is done of the heat regime over the do-main 3. 0×3. 5km^2at grids of 100×100 m in the hilly area of Zhaogongling located in thesouthern Dabishan Mountains. And for the first time maps are prepared for the Januaryand July mean temperature. Results suggest that the hilly-land temperature pattern de-pends heavily on the terrains in winter as compared to its much smaller effects in sum-mer.
出处
《南京气象学院学报》
CSCD
1992年第3期351-357,共7页
Journal of Nanjing Institute of Meteorology
基金
国家自然科学基金~~
关键词
丘陵山区
温度场
数值模拟
气温
hilly--land
temperature field
numerical simulation
