基于SPEI的近百年天津地区气象干旱时空演变特征 |
王敏, 尹义星, 陈晓旸, 郭阳, 徐梅, 罗传军 |
Changing characteristics of meteorological drought in Tianjin for almost one century based on standardized precipitation evapotranspiration index |
WANG Min, YIN Yixing, CHEN Xiaoyang, GUO Yang, XU Mei, LUO Chuanjun |
图5 春季(a)、夏季(b)、秋季(c)和冬季(d)天津地区SPEI[单位:10-1 (10 a)-1]、CRU-T [单位:℃·(10 a)-1]和GPCC-P[单位:mm·(10 a)-1]的气候倾向率空间分布[柱状向上(向下)代表气候倾向率为正(负), 6个柱状图依次代 |
Fig.5 The spatial distribution of climate tendency rate of SPEI [Unit: 10-1 (10 a)-1], CRU-T [Unit: ℃·(10 a)-1] and GPCC-P [Unit: mm·(10 a)-1] in spring (a), summer (b), autumn (c) and winter (d) in Tianjin region [up (down) columns represent positive (negative) climate tendency rate, six columns represent six periods in turn, and red dots represent MMK trend passing significant test] |
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