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Amazon drought and its implications for forest flammability and tree growth: a basin-wide analysis

机译:亚马逊干旱及其对森林易燃性和树木生长的影响:全流域分析

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Severe drought in moist tropical forests provokes large carbon emissions by increasing forest flammability and tree mortality, and by suppressing tree growth. The frequency and severity of drought in the tropics may increase through stronger El Nino Southern Oscillation (ENSO) episodes, global warming, and rainfall inhibition by land use change. However, little is known about the spatial and temporal patterns of drought in moist tropical forests, and the complex relationships between patterns of drought and forest fire regimes, tree mortality, and productivity. We present a simple geographic information system soil water balance model, called RisQue (Risco de Queimada - Fire Risk) for the Amazon basin that we use to conduct an analysis of these patterns for 1996-2001. RisQue features a map of maximum plant-available soil water (PAW(max)) developed using 1565 soil texture profiles and empirical relationships between soil texture and critical soil water parameters. PAW is depleted by monthly evapotranspiration (ET) fields estimated using the Penman-Monteith equation and satellite-derived radiation inputs and recharged by monthly rain fields estimated from 266 meteorological stations. Modeled PAW to 10 m depth (PAW(10 m)) was similar to field measurements made in two Amazon forests. During the severe drought of 2001, PAW(10 m) fell to below 25% of PAW(max) in 31% of the region's forests and fell below 50% PAW(max) in half of the forests. Field measurements and experimental forest fires indicate that soil moisture depletion below 25% PAW(max) corresponds to a reduction in leaf area index of approximately 25%, increasing forest flammability. Hence, approximately one-third of Amazon forests became susceptible to fire during the 2001 ENSO period. Field measurements also suggest that the ENSO drought of 2001 reduced carbon storage by approximately 0.2 Pg relative to years without severe soil moisture deficits. RisQue is sensitive to spin-up time, rooting depth, and errors in ET estimates. Improvements in our ability to accurately model soil moisture content of Amazon forests will depend upon better understanding of forest rooting depths, which can extend to beyond 15 m. RisQue provides a tool for early detection of forest fire risk.
机译:潮湿的热带森林中的严重干旱通过增加森林的易燃性和树木死亡率以及抑制树木生长而引起大量的碳排放。通过更强的厄尔尼诺南方涛动,全球变暖和土地利用变化抑制降雨,热带地区干旱的频率和严重性可能会增加。然而,人们对湿润热带森林干旱的时空格局以及干旱与森林火灾,树木死亡率和生产力之间的复杂关系知之甚少。我们提出了一个简单的地理信息系统土壤水分平衡模型,称为亚马逊河流域的RisQue(Risco de Queimada-火灾风险),我们用它来分析这些模式的1996-2001年。 RisQue绘制了一张地图,该地图使用1565种土壤质地剖面以及土壤质地与关键土壤水分参数之间的经验关系得出了最大植物可用土壤水(PAW(max))的图。 PAW被Penman-Monteith方程和卫星衍生的辐射输入估算的月蒸散量(ET)耗尽,并由266个气象站估算的月雨量补充。建模到10 m深度的PAW(PAW(10 m))与在两个亚马逊森林中进行的野外测量相似。在2001年的严重干旱期间,该地区31%的森林中PAW(10 m)降至PAW(max)的25%以下,一半森林中PAW(max)低于50%。野外测量和森林大火试验表明,土壤水分耗竭低于25%PAW(max)对应于叶面积指数减少约25%,从而增加了森林的可燃性。因此,在2001年ENSO期间,大约三分之一的亚马逊森林易燃。野外测量还表明,相对于没有严重土壤水分不足的年份,2001年的ENSO干旱使碳储量减少了约0.2 Pg。 RisQue对加速时间,生根深度和ET估计误差很敏感。我们对亚马逊森林土壤水分含量进行准确建模的能力的提高,将取决于对森林生根深度的更好理解,该生根深度可以延伸到15 m以上。 RisQue提供了一种用于早期发现森林火灾风险的工具。

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