Climate Change: A Regional Perspective - lead.org.pk · Anomaly”. •Most important...
Transcript of Climate Change: A Regional Perspective - lead.org.pk · Anomaly”. •Most important...
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Climate Change:A Regional Perspective
Dr. Furrukh Bashir
Meteorologist
Research and Development Division
1Summer School on Managing Shared River Basins
Connecting Science & Policy for Integrated Water Resources ManagementCOMSTECH Secretariat, Islamabad
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Copyrights: Earth Observing System
OVERVIEW• Indus Basin (1.12 million km2)• Spans in 4 countries• 65% of Pakistan is Indus Basin• Pakistan- an agriculture based economy • Producing surplus grains• Subsistence farming to corporate farming• > 200 million population• > 250 km3 runoff capacity with around
50 km3 discharge to Arabian Sea• Is Indus Basin a closed basin?
Copyrights: chimalaya.org
China (8%)
India (39%)
Afghanistan (6%)
Pakistan (47%)
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Daily Climatology of Pakistan (1960-2013) 3
Maximum Temperature Minimum TemperaturePrecipitation
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Copyrights: Earth Observing System
HYDROMETEOROLOGICAL CHALLENGES IN PAKISTAN
Karakoram Anomaly
Sep 2016, IWMI
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Melting Glaciers: An Indicator of Global Warming
• Global warming and the corresponding increase in energy flux towards the Earth surface have resulted in the retreat of mountain glaciers and continuous loss of ice worldwide.
• Climate Change Indicator (EPA)
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HKH Glaciers Eastern Hindukush, Western
Karakoram, and Northwestern Himalayan Glaciers
• Retreat rates of HKH glaciers are less than the global average and some are either stable or growing.
• This anomalous behavior, widely referred to as “The Karakoram Anomaly”.
• Most important hydrometeorological challenge in Pakistan
A view of Concordia at Baltoro Glacier from Broad peakPhoto Credit: Marco Bianchi Fotografo, [email protected]
Mount-K2, 2011
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The Karakoram Anomaly“I began to see glacier thickening and advancing that I had not observed in the 35 years of field work before.”
Kenneth Hewitt (a glaciologist at Wilfrid Laurier University, Waterloo, Canada.)
“Nowhere else on Earth could you find such a high concentration of surge-type glaciers.”
Christoph Mayer (a glaciologist at the Bavarian Academy of Sciences and Humanities in Munich, Germany.)
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Controversy “Many people use advancing Karakoram glaciers to deny
climate change or the overall ill health of Himalayan glaciers.”
Graham Cogley(a remote-sensing expert, Trent University, Peterborough, Canada.)
“They may be advancing, but this does not necessarily mean they are gaining mass.”
“To surge or not to surge may have little to do with climate trends.”
Frank Paul (a remote-sensing expert, University of Zurich, Switzerland.)
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Malanguti Glacier, Shimshal Valley(March 29, 2018)
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Yazgdil Glacier, Shimshal Valley(March 29, 2018)
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Yuskan Gardan Glacier, Shimshal ValleyKhordopin Glacier, Shimshal Valley
Khordopin Glacier, Shimshal Valley
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Lake Formation and Drainage on Virjerab River
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What we know of HKH Glaciers?
• Lack of long-term field investigation. • Rugged inaccessible terrain. • Long-term in-situ meteorological
observations are limited mainly to valley-based stations that are situated away from the glaciers. • Explanations of the Karakoram
anomaly have been based mainly on analyses of long-term temperature, precipitation, and river flow records.
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To bridge the gapProblem Statement
What knowledge is the scientific community missing about change in in-situ meteorological variables, which may help to investigate the causes of the Karakoram Anomaly more effectively?
Objective
Quantify assessment of the change in in-situ meteorological variables that are playing role in establishment of the Karakoram Anomaly.
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HKH POSITIVE MASS BALANCE
• Increase in Precipitation (Winter & Summer)• Decrease in River Inflows (Summer) • Positive Mass Balance (Summer and Annually)
DATA:
Monthly means of Synoptic Weather
Observations from valley floors from 1961 - 2011
Observations: Maximum, Minimum Temperature,
Dry Bulb Temperature, Relative Humidity, Surface
Pressure, Near-surface Wind Speed, Cloud Cover
Fraction, Precipitation
Derived Quantities: Net Radiation,
Evapotranspiration, and Climate Moisture Index
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Factors Facilitating Positive Mass Balance of a Glacier
Net Radiation Cloud Cover FractionTotal Seasonal Precipitation
Water Vapor Pressure
Wind Speed
River Inflow
Temperature
Potential Evaporation Climate Moisture Index
WinterSpringSummer
Autumn
Annual
Δ
10𝑦𝑟
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Another Controversy?
The Karakoram Anomaly
Extratropical Storm
Winter & Spring
Summer Monsoon
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Conclusions• An integrated signal • Interplay in energy, mass, and
momentum • Increases in water vapor,
cloudiness and precipitation, and decreases in net radiation, near surface wind speed, and potential evapotranspiration have resulted in a positivehydrologic mass balance at the annual scale. • HKH watersheds
Moisture surplus Energy deficient
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