Dr. Muhammad Hanif National Weather Forecasting Centre PMD, Islamabad Redistribution of Precipitation (Seasonal Shift) in Pakistan & Super Flood in Pakistan-2010.

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Dr. Muhammad Hanif National Weather Forecasting Centre PMD, Islamabad Redistribution of Precipitation (Seasonal Shift) in Pakistan & Super Flood in Pakistan-2010 PMD Pakistan Meteorological Department

PMD Pakistan Meteorological Department Meteorology SERVICES Hydrology Agro-meteorology/Drought Seismology

Weather Forecasting System of PMD Data Technique Skill Short Range Weather Forecasts (24 – 48 Hrs): accuracy 90% Medium Range Weather Forecasts (1 – 2 weeks): accuracy 70-80% Long Range/Seasonal Weather Forecasts (1 – 6 Months): Poor

80 Rain Gauge Stations Data Bank of PMD (CDPC) Weather Forecasting System of PMD Weather Stations/Observatories Network 50 AWS DATA

10-cm Doppler Radars 1- Lahore 2- Mangla QPM Radar 1- Sialkot 5-cm Wx. Surveillance Radars 1- Islamabad 3- D.I.Khan 4- Rahim Yar Khan 4- Karachi Radar Network of PMD Weather Forecasting System of PMD DATA

Satellite Ground Stations of PMD HRPT 1- Islamabad 2- Quetta FY-2 E/D 1- Islamabad Weather Forecasting System of PMD DATA

Products: Weather Forecasts Weather Forecasting System of PMD Rain Temps Winds

Information on Website Weather Forecasting System of PMD

Extreme Rainfall Flash Floods Monsoon Zone Flash Floods in KPK-2010 Climate: Rainfall Distribution

In 2007, Zhang et al detected the anthropogenic impact on Global Precipitation. They showed a latitudinal redistribution of mean Global Precipitation, indicating increasing precipitation at high latitudes and decreasing precipitation at lower latitudes. Latitudinal Redistribution of Precipitation in Pakistan

-- 22° N -- 30° N -- 38° N Latitudinal Redistribution of Precipitation in Pakistan

Previous Current Monsoon Precipitation Shift ( km West) Latitudinal Redistribution of Precipitation in Pakistan These areas required more attention for water management and to mitigate the flood disasters in the future

Monsoonal Rain Shift These areas required more attention for water management and to mitigate the flood disasters in the future

JanFebMarAprMayJunJulAugSepOctNovDec 100 mm ---- Monthly Rainfall Shift JanFebMarAprMayJunJulAugSepOctNovDec 100 mm ---- Climate: JanFebMarAprMayJunJulAugSepOctNovDec 100 mm ---- Climate: Climate: Climate:

JanFebMarAprMayJunJulAugSepOctNovDec 100 mm ---- Monthly Rainfall Shift JanFebMarAprMayJunJulAugSepOctNovDec 100 mm ---- Climate: JanFebMarAprMayJunJulAugSepOctNovDec 100 mm ---- Climate: DRY WET WETTEST DRY DRIER DRIEST Winter Monsoon Climate: Climate: Climate: Wet Dry

JanFebMarAprMayJunJulAugSepOctNovDec Rainfall Projected Climate: Wet PeriodDry Period 6 Months (Mar – Aug)…………… Wet Window 6 Months (Sep – Feb)…………… Dry Window Winter Monsoon

Latitudinal Redistribution of Precipitation in Pakistan Due to significant increase in SEASONAL and ANNUAL Precipitation in Pakistan, and the WESTWARD SHIFT ( km) of Monsoonal Rainfall; 1- Rainfall over the Catchment Areas of Eastern Rivers has decreased (moved away). 2- The Probability of occurrence of Heavy Rainfall Events, leading to FLASH FLOODS/FLOODS, would be HIGH over western rivers instead of eastern rivers of Pakistan in the future. 3- Northwest Pakistan (Central parts of KPK & North-western parts of Punjab) are Extremely Vulnerable to Flash Floods/Floods. Pakistan Super Flood: 2010

UN Secretary General Ban Ki-moon visits Sultan Colony, an Internally Displaced Persons’ camp, in Punjab on 15 August 2010 in Multan. UN described the disaster as unprecedented, with over a third of the country under water (Evan Schneider/UN via Getty Images) SUPER FLOOD (2010) in Pakistan: Very Heavy Rainfall 0ver NW Pakistan

Army helicopter evacuates stranded villagers in Nowshera, Pakistan on Friday, 30 July Boats & helicopters struggled to reach hundreds of thousands of villagers cut off by floods in northwest region, this has been the deadliest disaster to hit the region since 1929 SUPER FLOOD (2010) in Pakistan: Very Heavy Rainfall 0ver NW Pakistan

Flood victims evacuate their villages in Sukkur, Sindh province following days of heavy rain SUPER FLOOD (2010) in Pakistan: Very Heavy Rainfall 0ver NW Pakistan

An aerial view shows a damaged bridge washed out by the floods in Ghazi,5 August 2010 (REUTERS ) SUPER FLOOD (2010) in Pakistan: Very Heavy Rainfall 0ver NW Pakistan

Survivors walk in the flooded area of Baseera village, Multan, on 10 August (Arif Ali/AFP/Getty Images) SUPER FLOOD (2010) in Pakistan: Very Heavy Rainfall 0ver NW Pakistan

Khyber PK Pakistan received 70.5 % above Normal rainfall in the month of July, 2010 Khyber Pakhtoonkhwa received 179.1% above Normal rainfall in July, 2010 SUPER FLOOD (2010) in Pakistan: Very Heavy Rainfall 0ver NW Pakistan

Westerly Wave (Mid Latitude Weather Systems) Tracks of Monsoon & Winter Weather Systems Monsoon Monsoonal Zone SUPER FLOOD (2010) in Pakistan: Very Heavy Rainfall 0ver NW Pakistan

Very Heavy Rainfall occurred due to INTERACTION of 2 Weather Systems (Westerly Wave & Monsoonal Wave) over NW Pakistan. SUPER FLOOD (2010) in Pakistan: Very Heavy Rainfall 0ver NW Pakistan

Russian Heat North China Heat SE China Rain/LS Pakistan Flood July 2010: Disasters in Asia Due to ENSO-Cycle, the displacement (northward shift) of Subtropical HIGHS perturbed the Jet Stream, leading to Extreme Weather in Asia in July, Super Flood (July, 2010) of Pakistan, Extreme HEAT over Russia and Heavy Rains/Landslides over SE China were INTERLINKED. SUPER FLOOD (2010) in Pakistan: Very Heavy Rainfall 0ver NW Pakistan

Post Analysis of Subtropical Highs (Ridge): 500 mb HH H SUPER FLOOD (2010) in Pakistan: Very Heavy Rainfall 0ver NW Pakistan Subtropical HIGHS (cause of stable/normal climate) Jet Stream

H H H SUPER FLOOD (2010) in Pakistan: Very Heavy Rainfall 0ver NW Pakistan Post Analysis of Subtropical Highs (Ridge): 500 mb

H H H SUPER FLOOD (2010) in Pakistan: Very Heavy Rainfall 0ver NW Pakistan Post Analysis of Subtropical Highs (Ridge): 500 mb

H H H SUPER FLOOD (2010) in Pakistan: Very Heavy Rainfall 0ver NW Pakistan Post Analysis of Subtropical Highs (Ridge): 500 mb

H H H SUPER FLOOD (2010) in Pakistan: Very Heavy Rainfall 0ver NW Pakistan Post Analysis of Subtropical Highs (Ridge): 500 mb

H H H SUPER FLOOD (2010) in Pakistan: Very Heavy Rainfall 0ver NW Pakistan Post Analysis of Subtropical Highs (Ridge): 500 mb

H H H SUPER FLOOD (2010) in Pakistan: Very Heavy Rainfall 0ver NW Pakistan Post Analysis of Subtropical Highs (Ridge): 500 mb

H H H SUPER FLOOD (2010) in Pakistan: Very Heavy Rainfall 0ver NW Pakistan Post Analysis of Subtropical Highs (Ridge): 500 mb

H SUPER FLOOD (2010) in Pakistan: Very Heavy Rainfall 0ver NW Pakistan Winter: 2010/ Subtropical Highs (Ridge): 500 mb H H

L H Winter 2011: Cold & Dry with Dense Fog

The Displacement of Sub-Tropical HIGHS, due to current ENSO Cycle (La-Nina episode) caused; 1- Extreme Rainfall over NW Pakistan during Monsoon Season (2010). 2- Deficient Rainfall & Extreme Cold/Fog over Pakistan during Current Winter Season. It is difficult to present an overall indication of the potential impacts of Climate Change in Pakistan. However, the occurrence of recent Extreme Events such as Flood-2010, Deficient Rainfall in Winter and Current Dense and Prolonged Fog are enough to get an Alarming-Attention about a possible Climate Change in Pakistan, having direct and large impacts on several sectors of the society. THANKS