A comprehensive framework for integrating lake hypsography and function on a global scale

IF 24.1
Cristian Gudasz, Dominic Vachon, Yves T. Prairie
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Abstract

As climate change and nutrient pollution intensify, understanding how millions of lakes will respond to such forcings as a global or regional collective has become urgent and yet capturing their role in Earthʼs system remain neither conceptually unified nor empirically constrained. Here we introduce a framework that aggregates individual lake hypsography and functional attributes into composite lakes globally, across climate zones or 1-degree Earth system grid cells. We find that globally, lake shape mirrors land rather than ocean, with shallow areas dominating. This structure reveals systematic differences between glaciated and non-glaciated regions and between colder and warmer climate zones. At the 1-degree Earth system grid cells, composite lakes group into five distinct clusters. Globally, an estimated 43% of lake volume and sediment surface area lie within the mixed layer. A composite mixed layer volume-to-sediment-surface-area ratio reveals dominant water column influence and biogeochemical sensitivities, with strong contrasts across climates and glacial histories. The proposed framework advances quantifying and understanding the collective role of lakes across spatial scales in Earthʼs system. This Analysis presents a new framework that integrates lake hypsography and functional attributes at global and climatic scales, revealing key patterns in lake ecosystems and their responses to climate impacts.

Abstract Image

在全球尺度上整合湖泊地貌和功能的综合框架。
随着气候变化和营养物污染加剧,了解数百万湖泊将如何作为一个全球或区域集体对这些强迫作出反应已经变得迫在眉睫,然而,捕捉它们在地球系统中的作用既没有概念上的统一,也没有经验上的限制。在这里,我们引入了一个框架,将单个湖泊的地形和功能属性聚合到全球的复合湖泊中,跨越气候带或1度地球系统网格单元。我们发现,在全球范围内,湖泊的形状反映的是陆地而不是海洋,而且以浅水区为主。这一结构揭示了冰川区和非冰川区以及寒冷和温暖气候带之间的系统差异。在1度地球系统网格单元中,复合湖泊分为五个不同的集群。在全球范围内,估计有43%的湖泊体积和沉积物表面积位于混合层内。复合混合层体积-沉积物-表面积比揭示了主要的水柱影响和生物地球化学敏感性,在气候和冰川历史中具有强烈的对比。提出的框架促进了对湖泊在地球系统中跨空间尺度的集体作用的量化和理解。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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