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The influence of lateral flow on land surface fluxes in southeast Australia varies with model resolution

<p>Land surface models (LSMs) used in climate models typically represent surface hydrology as one-dimensional vertical fluxes, neglecting the lateral movement of water within and between grids. It is assumed that lateral flow of water has a negligible impact on land surface states at climate modelli...

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主要な著者: A. Devanand, J. P. Evans, A. J. Pitman, S. Pal, D. Gochis, K. Sampson
フォーマット: Artigo
言語:Inglês
出版事項: Copernicus Publications 2025-09-01
シリーズ:Hydrology and Earth System Sciences
オンライン・アクセス:https://hess.copernicus.org/articles/29/4491/2025/hess-29-4491-2025.pdf
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