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首页> 外文期刊>Climate >Climatization—Negligent Attribution of Great Salt Lake Desiccation: A Comment on Meng (2019)
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Climatization—Negligent Attribution of Great Salt Lake Desiccation: A Comment on Meng (2019)

机译:气候化-大盐湖干化的过失归因:《孟》评论(2019)

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摘要

A recent article reviewed data on Great Salt Lake (Utah) and concluded falsely that climate changes, especially local warming and extreme precipitation events, are primarily responsible for lake elevation changes. Indeed climatically influenced variation of net inflows contribute to huge swings in the elevation of Great Salt Lake (GSL) and other endorheic lakes. Although droughts and wet cycles have caused lake elevation changes of over 4.5 m, they have not caused a significant long-term change in the GSL stage. This recent article also suggests that a 1.4 °C rise in air temperature and concomitant increase in the lake’s evaporative loss is an important reason for the lake’s decline. However, we calculate that a 1.4 °C rise may have caused only a 0.1 m decrease in lake level. However, since 1847, the lake has declined 3.6 m and the lake area has decreased by ≈50%, despite no significant change in precipitation ( p = 0.52) and a slight increase, albeit insignificant, in river flows above irrigation diversions ( p = 0.085). In contrast, persistent water extraction for agriculture and other uses beginning in 1847 now decrease water flows below diversions by 39%. Estimates of consumptive water use primarily for irrigated agriculture in the GSL watershed suggest that approximately 85% (2500 km 2 ) of the reduced lake area can be attributed to human water consumption. The recent article’s failure to calculate a water budget for the lake that included extensive water withdrawals misled the author to focus instead on climate change as a causal factor for the decline. Stable stream flows in GSL’s headwaters, inadequate temperature increase to explain the extent of its observed desiccation, stable long-term precipitation, and the magnitude of increased water consumption from GSL together demonstrate conclusively that climatic factors are secondary to human alterations to GSL and its watershed. Climatization, in which primarily non-climatic processes are falsely attributed to climatic factors, is a threat to the credibility of hydrological science. Despite a recent suggestion to the contrary, pressure to support Earth’s rising human population—in the form of increasing consumption of water in water-limited regions, primarily to support irrigated agriculture—remains the leading driver of desiccation of inland waters within Earth’s water-limited regions.
机译:最近的一篇文章回顾了大盐湖(犹他州)的数据,并错误地得出结论,气候变化,尤其是局部变暖和极端降水事件,是造成湖高变化的主要原因。的确,受气候影响的净流入量变化导致大盐湖(GSL)和其他背胶湖泊的高度大幅波动。尽管干旱和潮湿的循环导致湖泊高程变化超过4.5 m,但它们并未在GSL阶段造成重大的长期变化。最近的这篇文章还表明,气温升高1.4°C并随之增加湖泊的蒸发损失,这是造成湖泊下降的重要原因。但是,我们计算出,升高1.4°C可能仅导致湖水位下降0.1 m。然而,自1847年以来,尽管降水量没有显着变化(p = 0.52)并且灌溉流量以上的河流流量略有增加(p = 0.52),该湖却减少了3.6 m,湖泊面积减少了约50%。 0.085)。相比之下,从1847年开始持续用于农业和其他用途的水提取,现在使流向分流以下的水量减少了39%。对GSL流域主要用于灌溉农业的耗水量的估算表明,减少的湖泊面积约有85%(2500 km 2)可归因于人类的用水量。最近的文章未能计算包括大量取水在内的湖泊的水预算,这误导了作者将注意力集中在气候变化上,将其作为下降的原因。 GSL上游水流稳定,温度升高不足以解释其观测到的干燥程度,稳定的长期降水以及GSL耗水量增加的幅度共同表明,气候因素是人类改变GSL及其流域的次要因素。气候变化主要将非气候过程错误地归因于气候因素,这对水文科学的信誉构成了威胁。尽管最近有相反的建议,但以有限的地区增加水的消耗(主要是支持灌溉农业)的形式来支持地球上不断增长的人口的压力仍然是限制地球内陆水域干燥的主要动力地区。

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