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Ecosystem biophysical memory in the southwestern North America climate system

机译:北美西南气候系统中的生态系统生物物理记忆

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To elucidate the potential role of vegetation to act as a memory source in the southwestern North America climate system, we explore correlation structures of remotely sensed vegetation dynamics with precipitation, temperature and teleconnection indices over 1982–2006 for six ecoregions. We found that lagged correlations between vegetation dynamics and climate variables are modulated by the dominance of monsoonal or Mediterranean regimes and ecosystem-specific physiological processes. Subtropical and tropical ecosystems exhibit a one month lag positive correlation with precipitation, a zero- to one-month lag negative correlation with temperature, and modest negative effects of sea surface temperature (SST). Mountain forests have a zero month lag negative correlation with precipitation, a zero–one month lag negative correlation with temperature, and no significant correlation with SSTs. Deserts show a strong one–four month lag positive correlation with precipitation, a low zero–two month lag negative correlation with temperature, and a high four–eight month lag positive correlation with SSTs. The ecoregion-specific biophysical memories identified offer an opportunity to improve the predictability of land–atmosphere interactions and vegetation feedbacks onto climate.
机译:为了阐明植被在北美西南气候系统中作为记忆源的潜在作用,我们探讨了六个生态区在1982-2006年间的遥感植被动态与降水,温度和遥相关指数的相关结构。我们发现,植被动力学与气候变量之间的滞后相关性受到季风或地中海地区的优势以及特定于生态系统的生理过程的调节。亚热带和热带生态系统与降水之间存在一个月滞后正相关,与温度之间呈零到一个月滞后负相关,并且海面温度(SST)的影响较小。山区森林与降水的零月滞后负相关,与温度之间的零至一个月滞后负相关,与海表温度没有显着相关。沙漠表现出与降水强的一到四个月滞后正相关,零到两个月的滞后与温度负相关,一个高的四个八月的滞后与SST正相关。所确定的特定于生态区域的生物物理记忆为改善土地-大气相互作用和植被对气候的反馈的可预测性提供了机会。

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