首页> 外文期刊>Quaternary Science Reviews: The International Multidisciplinary Review Journal >The Mexican Drought Atlas: Tree-ring reconstructions of the soil moisture balance during the late pre-Hispanic, colonial, and modern eras
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The Mexican Drought Atlas: Tree-ring reconstructions of the soil moisture balance during the late pre-Hispanic, colonial, and modern eras

机译:墨西哥干旱地图集:在西班牙裔前,殖民时期和现代晚期,树轮重建土壤水分的平衡

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Mexico has suffered a long history and prehistory of severe sustained drought. Drought over Mexico is modulated by ocean-atmospheric variability in the Atlantic and Pacific, raising the possibility for long-range seasonal climate forecasting, which could help mediate the economic and social impacts of future dry spells. The instrumental record of Mexican climate is very limited before 1920, but tree-ring chronologies developed from old-growth forests in Mexico can provide an excellent proxy representation of the spatial pattern and intensity of past moisture regimes useful for the analysis of climate dynamics and climate impacts. The Mexican Drought Atlas (MXDA) has been developed from an extensive network of 252 climate sensitive tree-ring chronologies in and near Mexico. The MXDA reconstructions extend from 1400 CE-2012 and were calibrated with the instrumental summer WA) self-calibrating Palmer Drought Severity Index (scPDSI) on a 0.5 degrees latitude/longitude grid extending over land areas from 14 to 34 degrees N and 75-120 degrees W using Ensemble Point-by-Point Regression (EPPR) for the 1944-1984 period. The grid point reconstructions were validated for the period 1920-1943 against instrumental gridded scPDSI values based on the fewer weather station observations available during that interval. The MXDA provides a new spatial perspective on the historical impacts of moisture extremes over Mexico during the past 600-years, including the Aztec Drought of One Rabbit in 1454, the drought of El Ano de Hambre in 1785-1786, and the drought that preceded the Mexican Revolution of 1909-1910.
机译:墨西哥历史悠久,历史悠久,持续干旱严重。墨西哥和墨西哥的干旱受到大西洋和太平洋海洋大气变化的影响,从而提高了进行长期季节性气候预报的可能性,这可能有助于调解未来干旱时期的经济和社会影响。墨西哥气候的仪器记录在1920年之前非常有限,但是从墨西哥古老的森林发展而来的树年轮年代可以很好地代表过去的水分状况的空间格局和强度,对分析气候动态和气候很有用。影响。墨西哥干旱地图集(MXDA)是由墨西哥及附近地区252个对气候敏感的树木年轮年代学的广泛网络开发而成的。 MXDA重建范围从1400年CE-2012年开始,并使用仪器夏季WA进行了校准。自校准Palmer干旱严重性指数(scPDSI)在纬度/经度为0.5度的网格上,范围从N到14至34度和75-120使用Ensemble点对点回归(EPPR)在1944年至1984年期间的W度。网格点重建在1920-1943年期间根据仪器化网格scPDSI值进行了验证,基于该间隔内可用的较少气象站观测值。 MXDA为过去600年来极端湿度对墨西哥的历史影响提供了新的空间视角,包括1454年一只兔子的阿兹台克人干旱,1785-1786年的El Ano de Hambre干旱以及之前的干旱1909-1910年的墨西哥革命。

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