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Just Add Water and the Colorado River Still Reaches the Sea

机译:只是加水,科罗拉多河仍流向大海

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A recent article in Environmental Management by All argued that flood flows in North America's Colorado River do not reach the Gulf of California because they are captured and evaporated in Laguna Salada, a below sea-level lakebed near the mouth of the river. We refute this hypothesis by showing that (1) due to its limited area, the Laguna Salada could have evaporated less than 10% of the flood flows that have occurred since 1989; (2) low flow volumes preferentially flow to the Gulf rather than Laguna Salada; (3) All's method for detecting water surface area in the Laguna Salada appears to be flawed because Landsat Thematic Mapper images of the lakebed show it to be dry when All's analyses said it was flooded; (4) direct measurements of salinity at the mouth of the river and in the Upper Gulf of California during flood flows in 1993 and 1998 confirm that flood waters reach the sea; and (5) stable oxygen isotope signatures in clam shells and fish otoliths recorded the dilution of seawater with fresh water during the 1993 and 1998 flows. Furthermore, All's conclusion that freshwater flows do not benefit the ecology of the marine zone is incorrect because the peer-reviewed literature shows that postlarval larval shrimp populations increase during floods, and the subsequent year's shrimp harvest increases. Furthermore, freshwater flows increase the nursery area for Gulf corvina (Cynoscion othonopterus), an important commercial fish that requires estuarine habitats with salinities in the range of 26-38‰ during its natal stages. Although flood flows are now much diminished compared to the pre-dam era, they are still important to the remnant wetland and riparian habitats of the Colorado River delta and to organisms in the intertidal and marine zone. Only a small fraction of the flood flows are evaporated in Laguna Salada.
机译:所有人在《环境管理》杂志上最近发表的一篇文章认为,北美科罗拉多河的洪水没有到达加利福尼亚湾,因为它们被拉古纳·萨拉达(Laguna Salada)捕获并蒸发了,拉古纳·萨拉达(Laguna Salada)在河口附近的海平面以下。我们通过证明这一假设来反驳这一点:(1)由于面积有限,拉古纳·萨拉达(Laguna Salada)蒸发的量可能少于1989年以来发生的洪水流量的10%; (2)低流量优先流向海湾而不是拉古纳·萨拉达; (3)All的检测Laguna Salada中水表面积的方法似乎存在缺陷,因为当All's分析称其被淹时,湖床的Landsat Thematic Mapper图像显示出它是干燥的; (4)在1993年和1998年洪水期间对河口和加利福尼亚上海湾的盐度进行直接测量,证实洪水已进入海洋; (5)蛤壳和鱼耳石中稳定的氧同位素特征记录了1993年和1998年水流中海水被淡水稀释的情况。此外,All的结论认为淡水流量无益于海洋区域的生态是不正确的,因为经过同行评审的文献显示,洪水期间幼虫后虾的数量增加,而下一年虾的收获量增加。此外,淡水的流动增加了湾美人鱼(Cynoscion othonopterus)的育苗面积,这是一种重要的商业鱼类,在其出生阶段需要河口栖息地的盐度范围为26-38‰。尽管与大坝前时期相比,洪水流量现在已大大减少,但它们对于科罗拉多河三角洲的残余湿地和河岸生境以及潮间带和海洋带的生物仍然很重要。拉古纳·萨拉达(Laguna Salada)仅蒸发了一小部分洪水。

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