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On the contribution of lakes in predicting near-surface temperature in a global weather forecasting model Cover

On the contribution of lakes in predicting near-surface temperature in a global weather forecasting model

Open Access
|Dec 2012

Figures & Tables

Fig. 1. 

Lake cover fraction as provided by the GLCC land-cover map.

Fig. 2. 

Global lake and oceans bathymetry (merged product described in the text).

Fig. 3. 

Climatological lake mixed-layer temperature [in K] in (a) winter (DJF), (b) spring (MAM), (c) summer (JJA), (d) autumn (SON) seasons as generated by the lake-planet simulations (1989–2009).

Fig. 4. 

As in Fig. 3 but lake ice depth [in m].

Fig. 5. 

Comparison between the lake-planet mixed-layer temperature simulations and the MODIS LST during the period 2001–2008 over grid points where the model lake fraction is greater than 10%.

Fig. 6. 

Comparison between the lake-planet ice simulation and IMS ice product: (a) ice formation day and (b) ice break-up day for three model ice-depth thresholds (1, 20 and 40 cm) are shown.

Fig. 7. 

Sensitivity of 48-hour T2m forecasts (valid at 00 UTC) for LAKE compared with NOLAKE for (a) winter (DJF) and (b) autumn (SON). Negative values indicate cooling.

Fig. 8. 

As in Fig. 7 but for (a) spring (MAM) and (b) summer (JJA).

Fig. 9. 

Impact of 48-hour T2m forecasts (valid at 00 UTC) for LAKE compared with NOLAKE, verified against the ECMWF T2m analysis: Mean Absolute Error difference for (a) winter (DJF) and (b) autumn (SON). Negative values indicate an improvement (MAE reduction).

Fig. 10. 

As in Fig. 9 but for (a) spring (MAM) and (b) summer (JJA).

Language: English
Page range: 15829 - 15829
Submitted on: May 17, 2011
Published on: Dec 1, 2012
Published by: Stockholm University Press
In partnership with: Paradigm Publishing Services

© 2012 G. Balsamo, R. Salgado, E. Dutra, S. Boussetta, T. Stockdale, M. Potes, published by Stockholm University Press
This work is licensed under the Creative Commons Attribution 4.0 License.