Simulated single-layer forest canopies delay Northern Hemisphere snowmelt
Single-layer vegetation schemes in modern land surface models have been found to overestimate diurnal cycles in longwave radiation beneath forest canopies. This study introduces an empirical correction, based on forest-stand-scale simulations, which reduces diurnal cycles of sub-canopy longwave radi...
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fttriple:oai:gotriple.eu:oai:doaj.org/article:f45c19f50a384d3c9de26de291a8080d 2023-05-15T18:32:17+02:00 Simulated single-layer forest canopies delay Northern Hemisphere snowmelt M. Todt N. Rutter C. G. Fletcher L. M. Wake 2019-11-01 https://doi.org/10.5194/tc-13-3077-2019 https://www.the-cryosphere.net/13/3077/2019/tc-13-3077-2019.pdf https://doaj.org/article/f45c19f50a384d3c9de26de291a8080d en eng Copernicus Publications doi:10.5194/tc-13-3077-2019 1994-0416 1994-0424 https://www.the-cryosphere.net/13/3077/2019/tc-13-3077-2019.pdf https://doaj.org/article/f45c19f50a384d3c9de26de291a8080d undefined The Cryosphere, Vol 13, Pp 3077-3091 (2019) envir geo Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2019 fttriple https://doi.org/10.5194/tc-13-3077-2019 2023-01-22T18:59:33Z Single-layer vegetation schemes in modern land surface models have been found to overestimate diurnal cycles in longwave radiation beneath forest canopies. This study introduces an empirical correction, based on forest-stand-scale simulations, which reduces diurnal cycles of sub-canopy longwave radiation. The correction is subsequently implemented in land-only simulations of the Community Land Model version 4.5 (CLM4.5) in order to assess the impact on snow cover. Nighttime underestimations of sub-canopy longwave radiation outweigh daytime overestimations, which leads to underestimated averages over the snow cover season. As a result, snow temperatures are underestimated and snowmelt is delayed in CLM4.5 across evergreen boreal forests. Comparison with global observations confirms this delay and its reduction by correction of sub-canopy longwave radiation. Increasing insolation and day length change the impact of overestimated diurnal cycles on daily average sub-canopy longwave radiation throughout the snowmelt season. Consequently, delay of snowmelt in land-only simulations is more substantial where snowmelt occurs early. Article in Journal/Newspaper The Cryosphere Unknown The Cryosphere 13 11 3077 3091 |
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English |
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envir geo |
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envir geo M. Todt N. Rutter C. G. Fletcher L. M. Wake Simulated single-layer forest canopies delay Northern Hemisphere snowmelt |
topic_facet |
envir geo |
description |
Single-layer vegetation schemes in modern land surface models have been found to overestimate diurnal cycles in longwave radiation beneath forest canopies. This study introduces an empirical correction, based on forest-stand-scale simulations, which reduces diurnal cycles of sub-canopy longwave radiation. The correction is subsequently implemented in land-only simulations of the Community Land Model version 4.5 (CLM4.5) in order to assess the impact on snow cover. Nighttime underestimations of sub-canopy longwave radiation outweigh daytime overestimations, which leads to underestimated averages over the snow cover season. As a result, snow temperatures are underestimated and snowmelt is delayed in CLM4.5 across evergreen boreal forests. Comparison with global observations confirms this delay and its reduction by correction of sub-canopy longwave radiation. Increasing insolation and day length change the impact of overestimated diurnal cycles on daily average sub-canopy longwave radiation throughout the snowmelt season. Consequently, delay of snowmelt in land-only simulations is more substantial where snowmelt occurs early. |
format |
Article in Journal/Newspaper |
author |
M. Todt N. Rutter C. G. Fletcher L. M. Wake |
author_facet |
M. Todt N. Rutter C. G. Fletcher L. M. Wake |
author_sort |
M. Todt |
title |
Simulated single-layer forest canopies delay Northern Hemisphere snowmelt |
title_short |
Simulated single-layer forest canopies delay Northern Hemisphere snowmelt |
title_full |
Simulated single-layer forest canopies delay Northern Hemisphere snowmelt |
title_fullStr |
Simulated single-layer forest canopies delay Northern Hemisphere snowmelt |
title_full_unstemmed |
Simulated single-layer forest canopies delay Northern Hemisphere snowmelt |
title_sort |
simulated single-layer forest canopies delay northern hemisphere snowmelt |
publisher |
Copernicus Publications |
publishDate |
2019 |
url |
https://doi.org/10.5194/tc-13-3077-2019 https://www.the-cryosphere.net/13/3077/2019/tc-13-3077-2019.pdf https://doaj.org/article/f45c19f50a384d3c9de26de291a8080d |
genre |
The Cryosphere |
genre_facet |
The Cryosphere |
op_source |
The Cryosphere, Vol 13, Pp 3077-3091 (2019) |
op_relation |
doi:10.5194/tc-13-3077-2019 1994-0416 1994-0424 https://www.the-cryosphere.net/13/3077/2019/tc-13-3077-2019.pdf https://doaj.org/article/f45c19f50a384d3c9de26de291a8080d |
op_rights |
undefined |
op_doi |
https://doi.org/10.5194/tc-13-3077-2019 |
container_title |
The Cryosphere |
container_volume |
13 |
container_issue |
11 |
container_start_page |
3077 |
op_container_end_page |
3091 |
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1766216379443183616 |