地理研究 ›› 2017, Vol. 36 ›› Issue (4): 743-754.doi: 10.11821/dlyj201704012
收稿日期:
2016-11-09
修回日期:
2017-02-12
出版日期:
2017-04-20
发布日期:
2017-04-20
作者简介:
作者简介:覃郑婕(1991- ),女,广西宜州人,硕士,研究方向为积雪遥感与气候变化。E-mail:
基金资助:
Zhengjie QIN1(), Shugui HOU1(
), Yetang WANG2, Hongxi PANG1
Received:
2016-11-09
Revised:
2017-02-12
Online:
2017-04-20
Published:
2017-04-20
摘要:
青藏高原积雪不仅是气候变化的敏感指示器,而且对亚洲季风区乃至全球气候具有显著影响。利用2002-2014年MODIS积雪覆盖范围产品及ERA-Interim再分析资料,采用气候统计诊断方法探究了青藏高原冬季积雪的时空变化特征及其与北极涛动(AO)的关系,结果表明:① 高原冬季积雪空间分布差异明显,高原西部和东南部多雪,中部和北部少雪,东部积雪年际变化大,西部多雪区积雪较为稳定。② 高原冬季积雪EOF分解第一模态具有东—西反位相变化特征,当高原东部积雪偏多(少)时,西部积雪偏少(多)。③ 该模态与AO密切相关。AO正位相时,东亚大槽减弱,南支槽加深东移,西太平洋副高加强使得更多暖湿气流到达高原,有利于高原东部降雪,而高原西南侧阿拉伯海附近存在反气旋异常,使得阿拉伯海的水汽不易抬升进入高原西部,高原西部盛行干燥的下沉气流异常,造成少雪的环流背景,且地表温度偏高不利于积雪维持,从而导致高原西部积雪的减少;AO负位相时,东亚大槽增强使得冬季风加强,高原东部受来自西北的干冷气流控制,不利于降雪产生,高原西南侧出现气旋异常,促使来自阿拉伯海和孟加拉湾的暖湿气流输送至高原西部,与来自西伯利亚的冷空气相遇,营造多雪的环流背景。
覃郑婕, 侯书贵, 王叶堂, 庞洪喜. 青藏高原冬季积雪时空变化特征及其与北极涛动的关系[J]. 地理研究, 2017, 36(4): 743-754.
Zhengjie QIN, Shugui HOU, Yetang WANG, Hongxi PANG. Spatio-temporal variability of winter snow cover over the Tibetan Plateau and its relation to Arctic Oscillation[J]. GEOGRAPHICAL RESEARCH, 2017, 36(4): 743-754.
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