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Page 1: Regional Climate Modelling over Southern Africa Mary-Jane M. Kgatuke

Regional Climate Modelling over Southern Africa

Mary-Jane M. Kgatuke

South African Weather Service

Page 2: Regional Climate Modelling over Southern Africa Mary-Jane M. Kgatuke

The effect of topography

CSIRO GCM TOPO

MAX TEMP MAX TEMP

DARLAM TOPO

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DARLAMCSIRO Atmospheric Research, Australia

Configuration over Africa

Africa 0º

30º

10º

20º

40º

0º 10º 20º 30º 40º 50º

100 x 100 grid points on a Lambert Conformal Projection(60x60 km resolution)

18 sigma layers in the vertical

Boundary values supplied by CSIRO9 (R21) AGCM – crosses

Semi-Lagragian advection & McGregor cumulus convection parameterization

Time step of 15 minutes integrating the hydrostatic equations forward in time

SIMULATES 30 DAYS IN 2 HOURS ON A LOCAL COMPUTER @ LRAM

Page 4: Regional Climate Modelling over Southern Africa Mary-Jane M. Kgatuke

Three 10-year regional model simulations forced by the global CSIRO-9 (R21) AGCM for the

A2 SRES scenario

2021 - 20301991 - 2000 2051 - 2060Basis climate

average over 10 years

REGIONAL SCALE CLIMATE CHANGE SCENARIO MODEL SIMULATIONS OVER SUB-

SAHARAH AFRICA

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January 2021 - 2030 January 2051 - 2060

MAX TEMP ANOMALY MAX TEMP ANOMALY

MIN TEMP ANOMALYMIN TEMP ANOMALY

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January 2021 - 2030 January 2051 - 2060

RAINFALL ANOMALY RAINFALL ANOMALY

MSLP ANOMALYMSLP ANOMALY

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Models

• Models tend to be set up according to the performance of physical parameterizations chosen to represent different processes.

• The performance of the models will be different and therefore it is necessary to use different models for the same target area.

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Models implemented in South Africa

• Regional climate studies– DARLAM at the University of Pretoria– RegCM2 at the South African Weather Service

• Short term forecasting at the South African Weather Service– ETA (operational)– MM5

Page 9: Regional Climate Modelling over Southern Africa Mary-Jane M. Kgatuke

RegCM2 over Southern Africa

• RegCM2 has been used to simulate tropical cyclone-like vortex tracks in the southern Indian Ocean

• Resolution:60 km

• Forcing fields: ECMWF

• Cumulus parameterization: Grell

• Time step :150 s

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Page 11: Regional Climate Modelling over Southern Africa Mary-Jane M. Kgatuke
Page 12: Regional Climate Modelling over Southern Africa Mary-Jane M. Kgatuke

Objectives of the project with RegCM3(1)

• Examine the skill of RegCM3 in simulating regional climate over southern Africa.

• Determine the extent to which the simulations are compromised by errors in predicted SST’s and GCM output.

• Determine if RegCM3 is capable of simulating the variability between wet and dry periods.

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Objectives of the project with RegCM3(2)

• Determine the skill of RegCM3 in capturing extreme rainfall events.

Page 14: Regional Climate Modelling over Southern Africa Mary-Jane M. Kgatuke

Thank you


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