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Coupled atmosphere-land model of the Arctic: Hirham5-CLM

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Work Plan, 29. 08 2012

Coupled atmosphere-land

model of the Arctic: Hirham5-CLM

Xu. Zhou, A. Rinke, H. Matthes, K. Dethloff

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Motivation

Improve land surface and atmosphere interactions in arctic region.

Understanding and representation of land surface processes. (permafrost and frozen ground affection to atmosphere circulation, atmospheric

impacts on land)

CLM (Community land model): More sophisticated biogeophysical and hydrological processes.

Improved vegetation dynamics.

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Land

Reference Height, Solar radiation, , long wave radiation, Lowest model level

temperature, Lowest model level pressure, Lowest model

level specific humidity, Lowest model level wind

speed, Precipitation Latent heat flux

Atmospheric forcing

Sensible heat flux Albedo (for short

wave radiation) Surface temperature

(for long wave radiation)

Surface energy

budget Temperature

Evaporation Humidity

Cloud water

CLM Hirham5

Hirham5-CLM couple(structure)

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Model setup for Hirham5 and Hirham5-CLM (HCLM)

⦁ Geographic location: Arctic region

⦁ Run time period: 1989-2011

⦁ Resolution: 25 km

⦁ Boundary forcing (EraInterim):

Surface pressure, Wind,

Temperature, Specific humidity, Cloud water, Cloud ice, Sea surface temperature, sea ice fraction

⦁ Surface data (for HCLM): Plant functional type (MODIS), Soil color (MODIS), Organic matter (WISE, HWSD), lake and wetland

(GLWD)...

Fig. 1. Integration area and orography [m]

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Improvement of land surface data: lake and wetland (from Global Lakes and Wetlands Database)

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Improvement of land surface data: Plant functional type (from Ncar, unreleased)

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Comparison of Hirham5 with HCLM for test run (monthly mean of 2002 March)

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Comparison of Hirham5 with HCLM for test run (monthly mean of 2002 March)

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Summary

⦁ Code of the Hirham5-CLM coupling finished.

⦁ New land surface data created. (Pfts, Percentage of Glacier, Lake and wetland, Soil color, Percentage of sand and clay, Organic matter)

⦁ Current work: Model restart.

⦁ Next step: Take longer (1 year) test run as soon as we finish model restart.

⦁ Evaluating the coupling by comparison with EraInterim data and observation data.

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The End!

Thank you!

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