植被-大气-海洋相互作用对中期全新纪气候的影响
Ganopolski1, Kubatzki, Claussen
1A. Ganopolski, C. Kubatzki, V. Brovkin, Potsdam-Institut fur Klimafolgenforschung, Postfach 601203, D-14412 Potsdam, Germany. M. Claussen, Potsdam-Institut fur Klimafolgenforschung, Postfach 601203, D-14412 Potsdam, Germany and Institut.
概括
中 Holocene 植被变化放大了北半球对太阳辐射的气候反应. 观察到协同效应,反因度而异,影响海洋循环和全球温度.
科学领域:
- 古气候学 古气候学
- 气候建模 气候建模
- 地球系统科学 地球系统科学
背景情况:
- 中期的全新世 (大约. 6000年前) 经历了北半球变化的太阳晒照.
- 在此期间,植被覆盖面发生了显著的变化.
- 了解过去的气候动态对于预测未来的气候变化至关重要.
研究的目的:
- 为了研究中期Holocene植被变化如何影响气候系统对季节性太阳辐射增强的反应.
- 量化植被覆盖对气候反的影响的直接和间接影响.
- 分析气候反机制的度变化.
主要方法:
- 使用同步合的大气-海洋-植被模型进行模拟.
- 专注于中 Holocene 时期与特定的太阳辐射条件.
- 分析了表面白度,海洋温度,海冰覆盖和海洋循环的变化.
主要成果:
- 植被变化直接 (通过白度) 和间接 (通过海洋过程) 改变和放大气候反应.
- 在北极度发现了植被,海洋温度和海冰之间的强烈协同效应.
- 大气-植被反在亚热带地区最为关键.
- 大西洋热环流减少导致南半球变暖.
结论:
- 植被覆盖是放大气候系统对阳光变化反应的重要因素.
- 在主要的气候反机制中存在度差异.
- 海洋循环的变化,就像热循环一样,对温度分布具有全球影响.
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