Evaluation of the snow regime in dynamic vegetation land surface models using field measurements

An increasing number of studies have demonstrated significant climatic and ecological changes occurring in the northern latitudes over the past decades. As coupled Earth-system models attempt to describe and simulate the dynamics and complex feedbacks of the Arctic environment, it is important to re...

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Published in:The Cryosphere
Main Authors: Kantzas, E., Quegan, S., Lomas, M., Zakharova, E.
Format: Other/Unknown Material
Language:English
Published: 2018
Subjects:
Online Access:https://doi.org/10.5194/tc-8-487-2014
https://tc.copernicus.org/articles/8/487/2014/
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spelling ftcopernicus:oai:publications.copernicus.org:tc20286 2023-05-15T15:09:55+02:00 Evaluation of the snow regime in dynamic vegetation land surface models using field measurements Kantzas, E. Quegan, S. Lomas, M. Zakharova, E. 2018-09-27 info:eu-repo/semantics/application/pdf https://doi.org/10.5194/tc-8-487-2014 https://tc.copernicus.org/articles/8/487/2014/ eng eng info:eu-repo/grantAgreement/EC/FP7/242446 doi:10.5194/tc-8-487-2014 https://tc.copernicus.org/articles/8/487/2014/ info:eu-repo/semantics/openAccess eISSN: 1994-0424 info:eu-repo/semantics/Text 2018 ftcopernicus https://doi.org/10.5194/tc-8-487-2014 2020-07-20T16:25:08Z An increasing number of studies have demonstrated significant climatic and ecological changes occurring in the northern latitudes over the past decades. As coupled Earth-system models attempt to describe and simulate the dynamics and complex feedbacks of the Arctic environment, it is important to reduce their uncertainties in short-term predictions by improving the description of both system processes and its initial state. This study focuses on snow-related variables and makes extensive use of a historical data set (1966–1996) of field snow measurements acquired across the extent of the former Soviet Union to evaluate a range of simulated snow metrics produced by several land surface models, most of them embedded in IPCC-standard climate models. We reveal model-specific failings in simulating snowpack properties such as magnitude, inter-annual variability, timings of snow water equivalent and evolution of snow density. We develop novel and model-independent methodologies that use the field snow measurements to extract the values of fresh snow density and snowpack sublimation, and exploit them to assess model outputs. By directly forcing the surface heat exchange formulation of a land surface model with field data on snow depth and snow density, we evaluate how inaccuracies in simulating snow metrics affect soil temperature, thaw depth and soil carbon decomposition. We also show how field data can be assimilated into models using optimization techniques in order to identify model defects and improve model performance. Other/Unknown Material Arctic Copernicus Publications: E-Journals Arctic The Cryosphere 8 2 487 502
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description An increasing number of studies have demonstrated significant climatic and ecological changes occurring in the northern latitudes over the past decades. As coupled Earth-system models attempt to describe and simulate the dynamics and complex feedbacks of the Arctic environment, it is important to reduce their uncertainties in short-term predictions by improving the description of both system processes and its initial state. This study focuses on snow-related variables and makes extensive use of a historical data set (1966–1996) of field snow measurements acquired across the extent of the former Soviet Union to evaluate a range of simulated snow metrics produced by several land surface models, most of them embedded in IPCC-standard climate models. We reveal model-specific failings in simulating snowpack properties such as magnitude, inter-annual variability, timings of snow water equivalent and evolution of snow density. We develop novel and model-independent methodologies that use the field snow measurements to extract the values of fresh snow density and snowpack sublimation, and exploit them to assess model outputs. By directly forcing the surface heat exchange formulation of a land surface model with field data on snow depth and snow density, we evaluate how inaccuracies in simulating snow metrics affect soil temperature, thaw depth and soil carbon decomposition. We also show how field data can be assimilated into models using optimization techniques in order to identify model defects and improve model performance.
format Other/Unknown Material
author Kantzas, E.
Quegan, S.
Lomas, M.
Zakharova, E.
spellingShingle Kantzas, E.
Quegan, S.
Lomas, M.
Zakharova, E.
Evaluation of the snow regime in dynamic vegetation land surface models using field measurements
author_facet Kantzas, E.
Quegan, S.
Lomas, M.
Zakharova, E.
author_sort Kantzas, E.
title Evaluation of the snow regime in dynamic vegetation land surface models using field measurements
title_short Evaluation of the snow regime in dynamic vegetation land surface models using field measurements
title_full Evaluation of the snow regime in dynamic vegetation land surface models using field measurements
title_fullStr Evaluation of the snow regime in dynamic vegetation land surface models using field measurements
title_full_unstemmed Evaluation of the snow regime in dynamic vegetation land surface models using field measurements
title_sort evaluation of the snow regime in dynamic vegetation land surface models using field measurements
publishDate 2018
url https://doi.org/10.5194/tc-8-487-2014
https://tc.copernicus.org/articles/8/487/2014/
geographic Arctic
geographic_facet Arctic
genre Arctic
genre_facet Arctic
op_source eISSN: 1994-0424
op_relation info:eu-repo/grantAgreement/EC/FP7/242446
doi:10.5194/tc-8-487-2014
https://tc.copernicus.org/articles/8/487/2014/
op_rights info:eu-repo/semantics/openAccess
op_doi https://doi.org/10.5194/tc-8-487-2014
container_title The Cryosphere
container_volume 8
container_issue 2
container_start_page 487
op_container_end_page 502
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