北极表面,云层和来自太空的辐射特性最近的趋势
1Cooperative Institute for Meteorological Satellite Studies, University of Wisconsin-Madison, 1225 West Dayton Street, Madison, WI 53706, USA. xuanjiw@ssec.wisc.edu
概括
北极的变暖趋势显示,春季和夏季的多云性增加,冬季降温时云层减少. 季节性云变化会影响表面温度,这与大规模的大气循环模式有关.
科学领域:
- 气候科学 气候科学
- 大气物理学 大气物理学
- 遥感 遥感 遥感 遥感
背景情况:
- 北极地区表现出复杂的气候动态,受温度,白度和云层覆盖的影响.
- 了解北极云层特性的季节性变化对于气候建模至关重要.
研究的目的:
- 从1982年到1999年,分析卫星推导的北极云和表面特性的趋势.
- 调查辐射平衡和大气循环对观察到的北极气候变化的影响.
主要方法:
- 利用卫星数据来推导北极上空的云和表面特性.
- 分析了1982-1999年期间的时间趋势.
- 与北极振荡指数相关的观测变化.
主要成果:
- 观察到北极的变暖,春夏增加云层,冬季降温,降低云层.
- 春天的云层增加了辐射平衡的表面温度和白色变化.
- 夏季,秋季和冬季云层强迫表明了降温趋势,这表明如果没有这些变化,气候变暖将会放大.
结论:
- 季节性云变化在调节北极表面温度变化方面发挥着重要作用.
- 观察到的北极气候趋势与大规模的大气循环 (北极振荡) 密切相关,而不是局部过程.
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