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首页> 外文期刊>International Journal of Climatology: A Journal of the Royal Meteorological Society >El Nino and Indian Ocean influences on Indonesian drought: implications for forecasting rainfall and crop productivity
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El Nino and Indian Ocean influences on Indonesian drought: implications for forecasting rainfall and crop productivity

机译:厄尔尼诺和印度洋对印度尼西亚干旱的影响:对预报降雨和作物生产力的影响

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摘要

Indonesia is impacted by severe droughts that cause major food shortages over much of the country, and have long been linked with El Nino events in the tropical Pacific Ocean. Despite seasonal forecasts based on relatively complex climate models, the 1997-1998 'El Nino of the century' was still followed by huge shortfalls in crop production (e.g. a loss of 3 million tons of rice in Java alone), reflecting the large gap that can exist between these forecasts and their actual utilization in agricultural planning. Alternatively, simple predictive models of rainfall and crop yields for Indonesia and other Indian Ocean rim countries have utilized an index of equatorial Pacific sea surface temperatures (Nino-3.4 SST), and related this index directly to indices of rainfall and crop productivity. However, these latter models have not included climatic information from the Indian Ocean, also implicated as a likely cause of drought in western Indonesia. Here we show that an index of Indian Ocean SSTs, when combined with the previously utilized Nino-3.4 SSTs, provides a significantly more accurate model of Sept-Dec drought (PDSI) over Java, Indonesia, than Nino-3.4 SSTs alone (ar(2) 64.5% vs 37.9%). Based solely on data for the month of August, this model provides the best tradeoff between model skill and adequate lead time for the Sept-Dec rice planting season. Such simple models can be used to generate readily usable early warning forecasts of drought and crop failure risk in Indonesia, particularly in the western part of the country that is most influenced by Indian Ocean climate variability. Copyright (c) 2008 Royal Meteorological Society.
机译:印度尼西亚受到严重干旱的影响,造成该国大部分地区严重的粮食短缺,长期以来一直与热带太平洋的厄尔尼诺现象有关。尽管基于相对复杂的气候模型进行了季节性预报,但在1997-1998年的“本世纪的厄尔尼诺现象”之后,作物产量仍然严重不足(例如仅爪哇就损失了300万吨大米),反映出这些预测与其在农业计划中的实际利用之间可能存在差异。另外,印度尼西亚和其他印度洋沿岸国家的降雨和作物单产的简单预测模型利用了赤道太平洋海表温度指数(Nino-3.4 SST),并将该指数直接与降雨和作物生产力指数相关。但是,这些后一种模式并未包括来自印度洋的气候信息,这也被认为是印度尼西亚西部干旱的可能原因。在这里,我们表明,与单独使用的Nino-3.4 SST相比,印度洋SST的索引与先前使用的Nino-3.4 SST的组合提供了印度尼西亚爪哇岛9月至12月干旱(PDSI)的精确得多的模型(ar( 2)64.5%和37.9%)。仅基于8月份的数据,此模型在9月至12月水稻种植季节的模型技巧和充足的交货时间之间提供了最佳平衡。这种简单的模型可用于生成易于使用的印度尼西亚干旱和作物歉收风险的预警预报,特别是在印度洋气候变化影响最大的该国西部地区。版权所有(c)2008皇家气象学会。

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