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Geoscientific Model Development An interactive open-access journal of the European Geosciences Union
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Volume 9, issue 6 | Copyright
Geosci. Model Dev., 9, 2167-2189, 2016
https://doi.org/10.5194/gmd-9-2167-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

Model experiment description paper 15 Jun 2016

Model experiment description paper | 15 Jun 2016

Determining lake surface water temperatures worldwide using a tuned one-dimensional lake model (FLake, v1)

Aisling Layden1,a, Stuart N. MacCallum2, and Christopher J. Merchant3 Aisling Layden et al.
  • 14 Rose Hill, Sligo, Ireland
  • 2School of Geosciences, University of Edinburgh, Grant Institute, The King's Buildings, West Mains Road, Edinburgh, EH9 3FE, UK
  • 3Dept. of Meteorology, University of Reading, Harry Pitt Building, 3 Earley Gate, P.O. Box 238, Whiteknights, Reading, RG6 6AL, UK
  • aformerly at: University of Edinburgh, School of Geosciences, Crew Building, Kings Buildings, West Main Rd, Edinburgh EH9 3JN, UK

Abstract. A tuning method for FLake, a one-dimensional (1-D) freshwater lake model, is applied for the individual tuning of 244 globally distributed large lakes using observed lake surface water temperatures (LSWTs) derived from along-track scanning radiometers (ATSRs). The model, which was tuned using only three lake properties (lake depth, snow and ice albedo and light extinction coefficient), substantially improves the measured mean differences in various features of the LSWT annual cycle, including the LSWTs of saline and high altitude lakes, when compared to the observed LSWTs. Lakes whose lake-mean LSWT persists below 1°C for part of the annual cycle are considered to be seasonally ice-covered. For trial seasonally ice-covered lakes (21 lakes), the daily mean and standard deviation (2σ) of absolute differences between the modelled and observed LSWTs are reduced from 3.07°C±2.25°C to 0.84°C±0.51°C by tuning the model. For all other trial lakes (14 non-ice-covered lakes), the improvement is from 3.55°C±3.20°C to 0.96°C±0.63°C. The post tuning results for the 35 trial lakes (21 seasonally ice-covered lakes and 14 non-ice-covered lakes) are highly representative of the post-tuning results of the 244 lakes.

For the 21 seasonally ice-covered lakes, the modelled response of the summer LSWTs to changes in snow and ice albedo is found to be statistically related to lake depth and latitude, which together explain 0.50 (R2adj, p = 0.001) of the inter-lake variance in summer LSWTs. Lake depth alone explains 0.35 (p = 0.003) of the variance.

Lake characteristic information (snow and ice albedo and light extinction coefficient) is not available for many lakes. The approach taken to tune the model, bypasses the need to acquire detailed lake characteristic values. Furthermore, the tuned values for lake depth, snow and ice albedo and light extinction coefficient for the 244 lakes provide some guidance on improving FLake LSWT modelling.

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With the availability of lake surface water temperature (LSWT) satellite data for 246 globally distributed large lakes, we tune a lake model, FLake, by varying 3 basic lake properties, shown to have the most influence over the modelled LSWTs. Tuning reduces the mean absolute difference (between model and satellite LSWTs) from an average of 3.38 ºC per day (untuned model) to 0.85 ºC per day (tuned model). The effect of several LSWT drivers, such as wind speed and lake depth are also demonstrated.
With the availability of lake surface water temperature (LSWT) satellite data for 246 globally...
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