1979—2016年青藏高原水汽收支的气候变化特征及其成因
齐冬梅, 李跃清, 周长艳, 陈超, 赖欣

Climate variation characteristics and causes of water vapor budget over the Tibetan Plateau during 1979—2016
Dongmei QI, Yueqing LI, Changyan ZHOU, Chao CHEN, Xin LAI
表3 青藏高原北、南部年及季节平均各边界净水汽输送、总输入、总输出及净收支量 (106 kg·s-1)
Table 3 Annual and seasonal average net water vapor transportations through every boundary, total inflow, total outflow and net water vapor budget in northern and southern parts of the Tibetan Plateau (unit: 106 kg·s-1
分区时期南边界西边界北边界东边界边界总输入边界总输出净收支
北部春季0.507.578.85-15.1116.92-15.111.81
夏季6.098.4313.02-15.0027.54-15.0012.54
秋季8.535.992.91-18.7017.43-18.70-1.27
冬季2.585.841.21-11.149.63-11.14-1.51
4.436.976.51-15.0017.91-15.002.91
南部春季10.3920.59-0.50-21.9030.98-22.408.58
夏季48.2513.19-6.09-14.2461.44-20.3341.11
秋季24.989.67-8.53-22.8834.65-31.413.24
冬季4.5911.11-2.58-15.5915.70-18.17-2.47
22.0713.64-4.43-18.6635.71-23.0912.62