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Megadroughts in Southwestern North America in ECHO-G Millennial Simulations and Their Comparison to Proxy Drought Reconstructions

机译:ECHO-G千禧年模拟中的北美西南部大旱灾及其与替代干旱重建的比较

摘要

Simulated hydroclimate variability in millennium-length forced transient and control simulations from the ECHAM and the global Hamburg Ocean Primitive Equation (ECHO-G) coupled atmosphere–ocean general circulation model (AOGCM) is analyzed and compared to 1000 years of reconstructed Palmer drought severity index (PDSI) variability from the North American Drought Atlas (NADA). The ability of the model to simulate megadroughts in the North American southwest is evaluated. (NASW: 25°–42.5°N, 125°–105°W). Megadroughts in the ECHO-G AOGCM are found to be similar in duration and magnitude to those estimated from the NADA. The droughts in the forced simulation are not, however, temporally synchronous with those in the paleoclimate record, nor are there significant differences between the drought features simulated in the forced and control runs. These results indicate that model-simulated megadroughts can result from internal variability of the modeled climate system rather than as a response to changes in exogenous forcings. Although the ECHO-G AOGCM is capable of simulating megadroughts through persistent La Niña–like conditions in the tropical Pacific, other mechanisms can produce similarly extreme NASW moisture anomalies in the model. In particular, the lack of low-frequency coherence between NASW soil moisture and simulated modes of climate variability like the El Niño–Southern Oscillation, Pacific decadal oscillation, and Atlantic multidecadal oscillation during identified drought periods suggests that stochastic atmospheric variability can contribute significantly to the occurrence of simulated megadroughts in the NASW. These findings indicate that either an expanded paradigm is needed to understand multidecadal hydroclimate variability in the NASW or AOGCMs may incorrectly simulate the strength and/or dynamics of the connection between NASW hydroclimate variability and the tropical Pacific.
机译:分析了ECHAM和全球汉堡海洋原始方程(ECHO-G)耦合的大气-海洋总循环模型(AOGCM)进行的千年长度强迫瞬变和控制模拟中的模拟气候变化,并将其与1000年重建的Palmer干旱严重度指数进行了比较(PDSI)变异来自北美干旱地图集(NADA)。评估了该模型模拟北美西南部大旱灾的能力。 (NASW:25°–42.5°N,125°–105°W)。发现ECHO-G AOGCM中的特大干旱的持续时间和大小与NADA估计的相似。但是,强迫模拟中的干旱与古气候记录的干旱在时间上是不同步的,在强迫和控制运行中模拟的干旱特征之间也没有显着差异。这些结果表明,模型模拟的大干旱可能是由模拟气候系统的内部变化引起的,而不是对外源强迫变化的响应。尽管ECHO-G AOGCM能够通过热带太平洋上持续的拉尼娜现象模拟大干旱,但其他机制也会在该模型中产生类似的极端NASW湿度异常。特别是,在确定的干旱期间,NASW土壤水分与模拟的气候变异模式(如厄尔尼诺-南方涛动,太平洋年代际振荡和大西洋多年代际振荡)之间缺乏低频连贯性,这表明随机的大气变异性可以显着影响气候变化。在NASW中发生模拟大干旱。这些发现表明,需要一种扩展的范式来理解NASW的多年代际水文气候变化,否则AOGCM可能会错误地模拟NASW水文气候变化与热带太平洋之间联系的强度和/或动力学。

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