World Meteorological Organization Working together in weather climate

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World Meteorological Organization Working together in weather, climate and water WMO Impacts of Climate

World Meteorological Organization Working together in weather, climate and water WMO Impacts of Climate Change on water related risks AVINASH TYAGI Director, Climate and Water Department WORLD METEOROLOGICAL ORGANISATION Session 1. 3. 3: Managing water related risks in changing climate Fifth World Water Forum 16 -22 March, 2009, Istanbul, TURKEY WMO: Climate and Water Department www. wmo. int

Introduction

Introduction

What is global warming? “Global warming” refers to increases in global temperatures as a

What is global warming? “Global warming” refers to increases in global temperatures as a result of an accumulation of greenhouse gases in the atmosphere. Greenhouse gases, such as CO 2 , CH 4, N 2 O, HFCS, …

Potential Impacts of Climate Change Air temperature Sea level rise Precipitation form, timing and

Potential Impacts of Climate Change Air temperature Sea level rise Precipitation form, timing and quantity

OBSERVATIONS

OBSERVATIONS

Global mean temperatures Warmest 12 years: 1998, 2005, 2003, 2002, 2004, 2006, 2001, 1997,

Global mean temperatures Warmest 12 years: 1998, 2005, 2003, 2002, 2004, 2006, 2001, 1997, 1995, 1999, 1990, 2000 Period Rate 50 0. 128 0. 026 100 0. 074 0. 018 Years /decade

Sea level in 20 th century SPM-3 b Rates of sea level rise: •

Sea level in 20 th century SPM-3 b Rates of sea level rise: • 1. 8 + 0. 5 mm yr-1, 1961 -2003 • 1. 7 + 0. 5 mm yr-1, 20 th Century • 3. 1 + 0. 7 mm yr-1, 1993 -2003

Changes in Land precipitation Increases Decreases Smoothed annual anomalies for precipitation (%) over land

Changes in Land precipitation Increases Decreases Smoothed annual anomalies for precipitation (%) over land from 1900 to 2005; other regions are dominated by variability.

Wet Season Dry Season Source: Boer et al (2007) Between 18 and 21 mm/yr

Wet Season Dry Season Source: Boer et al (2007) Between 18 and 21 mm/yr Between 21 and 27 mm/yr Between 27 and 30 mm/yr Between 30 and 36 mm/yr Between -21 and -24 mm/yr Between -18 and -21 mm/yr Between -15 and -18 mm/yr Between -9 and -12 mm/yr Between -6 and -9 mm/yr Between -3 and -6 mm/yr Between 0 and -3 mm/yr

Effects on the hydrological cycle • Precipitations • Evaporation • Soil moisture • •

Effects on the hydrological cycle • Precipitations • Evaporation • Soil moisture • • Glaciers Streamflow • Groundwater • Floods • Low flows • Water Demand

Base flows in rivers Ciliwung Larona Barito Source: Water R&D Center, Bandung (2007).

Base flows in rivers Ciliwung Larona Barito Source: Water R&D Center, Bandung (2007).

Perth inflows

Perth inflows

Runoff from Finland:

Runoff from Finland:

Potential Impacts • All major socio-economic sectors will be affected, with a wide range

Potential Impacts • All major socio-economic sectors will be affected, with a wide range of regional impacts: – – – Water Ecosystems Food Coastal systems and low-lying areas Industry, settlement and society Health

Global warming will hit through water • Through climate change and the effects of

Global warming will hit through water • Through climate change and the effects of e. g… - changes in the hydrological cycle and water balance - sea level rise - increased water temperatures • Through increased climate variability in the form of more serious and frequent extremes, such as floods and droughts Source: TJK

Increasing number of hydrological extremes • Meuse river, December 1993 • Rhine river (secondary

Increasing number of hydrological extremes • Meuse river, December 1993 • Rhine river (secondary channel in floodplain), August 2003

Changes in major floods 1950 -2000 There’s a consistent 50 -year upward trend in

Changes in major floods 1950 -2000 There’s a consistent 50 -year upward trend in every region except Oceania.

Flood damages are increasing

Flood damages are increasing

Relative Vulnerability of coastal deltas

Relative Vulnerability of coastal deltas

Demographic Changes

Demographic Changes

Reasons for changes in flood risk and vulnerability Land-use change, increasing exposure and damage

Reasons for changes in flood risk and vulnerability Land-use change, increasing exposure and damage potential – floodplain development, growing wealth in flood-prone areas (ii) Changes in Land-cover change - urbanization, terrestrial systems deforestation, elimination of wetlands and floodplains, river regulation (iii) Changes in Holding capacity of the atmosphere, climate and intense precipitation, seasonality, atmospheric circulation patterns system Source: Kundzewicz & Schellnhuber, 2004 (i) Changes in socio-economic systems

PROJECTIONS

PROJECTIONS

21 st Century Is this going to be the flood century? (Too much water

21 st Century Is this going to be the flood century? (Too much water )

…or the drought century?

…or the drought century?

Probability distributions: temperatures (Adapted from Climate – Into the 21 st Century, WMO, 2003,

Probability distributions: temperatures (Adapted from Climate – Into the 21 st Century, WMO, 2003, Cambridge University Press)

Hazards – Floods – Droughts – Flow regime changes

Hazards – Floods – Droughts – Flow regime changes

“Climate change: the hydrologic cycle” changes in the averages/ trends changes in variability (magnitude,

“Climate change: the hydrologic cycle” changes in the averages/ trends changes in variability (magnitude, severity, duration)

General Circulation Models (GCMs) to estimate future climate variables. Due to model uncertainty, an

General Circulation Models (GCMs) to estimate future climate variables. Due to model uncertainty, an ensemble of models is more accurate than any single model. Temperature projections are much better than precipitation projections. AOGCMs • discretise the equations of fluid motion • parameterize processes at the subgrid scale. Climate Impacts Group (2007) GCMs are constantly improving, and converging to observations. Reichler and Kim (2007) BAMS

Annual mean changes of precipitation, soil moisture, runoff and evaporation (2080 -2099 relative to

Annual mean changes of precipitation, soil moisture, runoff and evaporation (2080 -2099 relative to 1980 -1999) Figure 10. 12 SRES A 1 B scenario AR 4 WGI Fig. 10. 12

Changes in extremes AR 4 WGI Fig. 10. 18 2080– 2099 minus 1980– 1999

Changes in extremes AR 4 WGI Fig. 10. 18 2080– 2099 minus 1980– 1999 for the A 1 B scenario annual total precipitation / number of wet days annual maximum number of consecutive dry days

Climate change on NZ east coast: Unirrigated drought risk, 2080 s “Low-medium” scenario “Medium-high”

Climate change on NZ east coast: Unirrigated drought risk, 2080 s “Low-medium” scenario “Medium-high” scenario

Coastal flooding Change from the present day to the 2080 s Unmitigated emissions Stabilisation

Coastal flooding Change from the present day to the 2080 s Unmitigated emissions Stabilisation at 750 ppm Stabilisation at 550 ppm

Changes in river runoff from the present day to the 2080 s Unmitigated emissions

Changes in river runoff from the present day to the 2080 s Unmitigated emissions Stabilisation of CO 2 at 750 ppm Change in annual runoff (%) Hadley Center Stabilisation of CO 2 at 550 ppm – 75 – 50 – 25 – 5 to 5 25 50 75 99/812 35

Downscaling from Global to Basin Levels We must downscale GCM data to an appropriate

Downscaling from Global to Basin Levels We must downscale GCM data to an appropriate resolution for hydrological predictions.

Resistance Strategies “Resistance” strategies focus mainly on the hazard (flood, drought, etc. ) by

Resistance Strategies “Resistance” strategies focus mainly on the hazard (flood, drought, etc. ) by aiming at prevention

Rainwater Harvesting: Reservoir in a building

Rainwater Harvesting: Reservoir in a building

DEMAND Management More efficient irrigation systems

DEMAND Management More efficient irrigation systems

Climate Alert System (CAS) Examples Seasonal climate forecast anomalies Climate monitoring Malaria monitoring at

Climate Alert System (CAS) Examples Seasonal climate forecast anomalies Climate monitoring Malaria monitoring at sentinel sites Year 1 Year 2 Year 3 Year 4 Climate Alert: low precip sets stage Climate Alert: high precip may trigger High precip; sentinels activated

Monthly, Seasonal, Interannual Monitoring

Monthly, Seasonal, Interannual Monitoring

El Niño and La Niña El Niño (1997) La Niña (1988)

El Niño and La Niña El Niño (1997) La Niña (1988)

Regional Climate Outlook Forums GHACOF: Greater Horn of Africa COF SARCOF: Southern Africa COF

Regional Climate Outlook Forums GHACOF: Greater Horn of Africa COF SARCOF: Southern Africa COF PRESAO: Prévision Saisonnière en Afrique de l’Ouest PRESAC: Prévision Saisonnière en Afrique Centrale FOCRAII: Forum On regional Climate monitoring, assessment and prediction for Regional Association II (Asia) SSACOF: Southeast of South America COF WCSACOF: Western Coast of South America COF CCOF: Caribbean COF FCCA: Foro Regional del Clima de América Central PICOF: Pacific Islands COF SEECOF: South. Eastern Europe COF

Thank you

Thank you

Maximum Temperature Minimum Temperature SOurce: Boer et al (2007) <0. 04 o. C/year Betweem

Maximum Temperature Minimum Temperature SOurce: Boer et al (2007) <0. 04 o. C/year Betweem 0. 04 and 0. 07 o. C/year > 0. 07 o. C/year <0. 04 o. C/year Between 0. 04 and 0. 07 o. C/year > 0. 07 o. C/year