Empirical modeling of summer lake surface temperatures in southwest Greenland

This work presents a method to estimate mean daily lake surface water temperatures using only air temperature, theoretical clear-sky solar radiation, and lake size. Surface water temperatures were measured at a selection of lakes in southwest Greenland during the summers of 1998–2000. The lakes are...

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Published in:Limnology and Oceanography
Main Authors: Kettle, Helen, Thompson, Roy, Anderson, N. John, Livingstone, David M.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2004
Subjects:
Online Access:https://doi.org/10.4319/lo.2004.49.1.0271
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spelling fteawag:oai:dora:eawag_4681 2023-05-15T16:28:13+02:00 Empirical modeling of summer lake surface temperatures in southwest Greenland Kettle, Helen Thompson, Roy Anderson, N. John Livingstone, David M. 2004 https://doi.org/10.4319/lo.2004.49.1.0271 eng eng Wiley Limnology and Oceanography--Limnol. Oceanogr.--journals:1929--0024-3590 eawag:4681 journal id: journals:1929 issn: 0024-3590 ut: 000188381100029 local: 9367 scopus: 2-s2.0-0742267777 doi:10.4319/lo.2004.49.1.0271 Text Journal Article 2004 fteawag https://doi.org/10.4319/lo.2004.49.1.0271 2023-04-09T04:48:01Z This work presents a method to estimate mean daily lake surface water temperatures using only air temperature, theoretical clear-sky solar radiation, and lake size. Surface water temperatures were measured at a selection of lakes in southwest Greenland during the summers of 1998–2000. The lakes are small (surface area <150 ha) with maximum depths ranging from 3.5 to 47 m. An empirical model requiring only local air temperature and theoretical clear-sky solar radiation is developed to predict daily mean lake surface temperatures in summer for each lake. The model approximates the slow integrated response of water temperature to meteorological forcing by applying an exponential smoothing filter to air temperature. Exponential smoothing results in a 35% improvement in model fit compared with a model using unsmoothed air temperatures. The smoothed air temperatures and clear-sky solar radiation are linearly combined to estimate the daily mean lake surface temperatures. The smoothing parameters and the three linear coefficients of the model, obtained individually for each of 15 lakes, are found to relate to lake area and maximum depth, leading to the development of a general model. With this general model it is possible to predict the summer surface temperatures at any lake in this region where local air temperatures can be estimated. Cross-validation of the general model at each lake in turn indicated a 90% forecast skill and average standard error of prediction of 1.0°C. Examination of the daily prediction errors over time suggests a relation to strong wind events. Article in Journal/Newspaper Greenland DORA Eawag Greenland Limnology and Oceanography 49 1 271 282
institution Open Polar
collection DORA Eawag
op_collection_id fteawag
language English
description This work presents a method to estimate mean daily lake surface water temperatures using only air temperature, theoretical clear-sky solar radiation, and lake size. Surface water temperatures were measured at a selection of lakes in southwest Greenland during the summers of 1998–2000. The lakes are small (surface area <150 ha) with maximum depths ranging from 3.5 to 47 m. An empirical model requiring only local air temperature and theoretical clear-sky solar radiation is developed to predict daily mean lake surface temperatures in summer for each lake. The model approximates the slow integrated response of water temperature to meteorological forcing by applying an exponential smoothing filter to air temperature. Exponential smoothing results in a 35% improvement in model fit compared with a model using unsmoothed air temperatures. The smoothed air temperatures and clear-sky solar radiation are linearly combined to estimate the daily mean lake surface temperatures. The smoothing parameters and the three linear coefficients of the model, obtained individually for each of 15 lakes, are found to relate to lake area and maximum depth, leading to the development of a general model. With this general model it is possible to predict the summer surface temperatures at any lake in this region where local air temperatures can be estimated. Cross-validation of the general model at each lake in turn indicated a 90% forecast skill and average standard error of prediction of 1.0°C. Examination of the daily prediction errors over time suggests a relation to strong wind events.
format Article in Journal/Newspaper
author Kettle, Helen
Thompson, Roy
Anderson, N. John
Livingstone, David M.
spellingShingle Kettle, Helen
Thompson, Roy
Anderson, N. John
Livingstone, David M.
Empirical modeling of summer lake surface temperatures in southwest Greenland
author_facet Kettle, Helen
Thompson, Roy
Anderson, N. John
Livingstone, David M.
author_sort Kettle, Helen
title Empirical modeling of summer lake surface temperatures in southwest Greenland
title_short Empirical modeling of summer lake surface temperatures in southwest Greenland
title_full Empirical modeling of summer lake surface temperatures in southwest Greenland
title_fullStr Empirical modeling of summer lake surface temperatures in southwest Greenland
title_full_unstemmed Empirical modeling of summer lake surface temperatures in southwest Greenland
title_sort empirical modeling of summer lake surface temperatures in southwest greenland
publisher Wiley
publishDate 2004
url https://doi.org/10.4319/lo.2004.49.1.0271
geographic Greenland
geographic_facet Greenland
genre Greenland
genre_facet Greenland
op_relation Limnology and Oceanography--Limnol. Oceanogr.--journals:1929--0024-3590
eawag:4681
journal id: journals:1929
issn: 0024-3590
ut: 000188381100029
local: 9367
scopus: 2-s2.0-0742267777
doi:10.4319/lo.2004.49.1.0271
op_doi https://doi.org/10.4319/lo.2004.49.1.0271
container_title Limnology and Oceanography
container_volume 49
container_issue 1
container_start_page 271
op_container_end_page 282
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