Leeds Omani Society

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• Leeds Omani Society
• 06 May 2006
• Juma Al-Maskari
• juma_at_env.leeds.ac.uk

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???? ????????? ??????? ?? ??????? http//alhawza.
net/forum
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Stages of a thunderstorm
Developing
Mature
Disipating
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Global observation network
Surface

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Upper Air
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AIST Super Cluster

• P-32 Cluster
• Number of nodes 1074 (Two CPUs for each
  node)Peak performance 8.59TFLOPSMain memory
  6GB/node (Total Main memory 6444GB)

Laptop memory 500 MB 1 GB
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Global grid (100 km resolution)
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A zoom into the area
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Oman

• Resolution 28 km upper image
• Resolution 7 km lower image
• Simplified equations.
• Good but not the best.

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Why ?
?Why ?

• Summer orographic convection over the Hajar
• Mountains causes flash floods, strong downdrafts,
• and sometimes hail.
• There is a need to understand the causes and
• therefore improve the ability to forecast.

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Observational Experiment
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Total Precipitation as forecasted by the Met
Office model for the 12 July 04 00UTC ? 15h
(1900 hours local time)
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Accumulated precipitation (mm), red dots
represent positions of rain-gauges with
precipitations
Total domain rainfall 6.7013 e3
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??????? ?????? ?? ????www.met.gov.om

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Something to take away

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• http//uk.weather.com/weather/local/UKXX0078
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• http//www.met.gov.om
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• http//www.kanzalarb.com
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