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5 – 6 October 2012, Bratislava, Slovakia
   Integrated Drought Management Programme in Central and Eastern Europe
             A GWP and WMO initiative: Regional Workshop Agenda




                               5 October 2012
Drought management: current status and future
regional perspectives, water management and
       agriculture sectors perspectives
Water scarcity and climate uncertainty; what do we know
                 on droughts in Europe

Dr. Elena Mateescu - National Meteorological Administration, Romania
Liviu Popescu – GWP, Romania
Outline
 Water scarcity and drought concepts
 Water scarcity, drought and CC - policy framework
 Knowledge base and information exchange on CC and drought –
  technical and scientific platform
 Climatic conditions in Europe – current status and projected changes
 Potential impacts of CC on the status of water resources in drought
  conditions
 What are the main sources of uncertainty on CC and drought impact ?
 Examples of information networks on DROUGHT
 Drought management and adaptation options – IDMP
 Conclusions
Water scarcity and drought concepts

     Water scarcity is a man-made caused phenomenon. It is a recurrent imbalance that arises
  from an overuse of water resources, caused by consumption being significantly higher than
  the natural renewable availability. Water scarcity can be more aggravated by disturbed
  meteorological conditions during drought episodes and even more complicated by the water
  pollution which is associated with lack of resources (reducing the suitability for different
  water uses);
     Drought is a natural phenomenon. It is a temporary, negative and severe deviation along a
  significant time period and over a large region from average precipitation values (a rainfall
  deficit), which might lead to meteorological, agricultural, hydrological and socio-economic
  drought, depending on its severity and duration (EU definitions on WS&D Report, 2007).

                                                                      TIME SCALE
                                            Short-term           Mid-term (months,     Long-term
                                          (days, weeks)           seasons, years)      (decades)
      Causes              Natural            Dry spell                 Drought           Aridity

                        Man-made         Water shortage             Water scarcity   Desertification

         Timescale and causes of water scarcity, drought and related concepts

    Source: Gap Analysis of the Water Scarcity and Droughts Policy in the EU,
    European Commission Tender ENV.D.1/SER/2010/0049                                  August 2012
Water scarcity, drought and CC – policy framework
Related on water scarcity and droughts policy, several EU policies and initiatives
contribute to efforts for adaptation to climate change impact on water resources
management; examples :
EU Water Framework Directive (WFD/2000/60/EC) and the Water Scarcity and
Droughts EU Policy (EC 2007b) refers :
          - to protect and restore the water environment across Europe by 2015 and to
          ensure the long term sustainable use of water;
          - to development of adaptation measures and sets out of a number of policy
options for addressing impacts of water scarcity and droughts in next decades.
 The Blueprint to safeguard Europe's water resources is a communication to be
released by the end of 2012 that will address the evolution of water resources, including
water's vulnerability to climate change and anthropogenic pressures (i.e. land use
management). It will focus on different water resource management aspects that are related
to adaption (land use management including forests, indicative water efficiency targets,
economic instruments, innovation, governance and knowledge base).
             WATER SAVING SHOULD BECAME THE PRIORITY.
 Drought Management Plans must be the first set of policy options for future action
Knowledge base and information exchange on CC and
   drought – technical and scientific platform
The White Paper of the European Commission “Adapting to climate change: Towards
a European framework for action” (COM/2009/147) issued in April 2009 sets out a framework
to reduce the EU’s areas vulnerability to the water scarcity and drought.
Starting with March 2012, the European Climate Adaptation Platform (CLIMATE- ADAPT)
is a publicly accessible web-based platform designed to support policy-makers at EU,
national, regional and local level in the development of climate change adaptation measures
and policies;
 The CLIMATE-ADAPT have been developed with the support of the European scientific and
policy making community, and will help users to access, disseminate and integrate information
on:
           - Expected climate change in Europe
           - The vulnerability of regions and sectors at present and in the future
           - National, regional and transnational adaptation activities and strategies
           - Case examples of adaptation and potential future adaptation options
           - Online tools that support adaptation planning
           - Adaptation-related research projects, guideline documents,
           reports information sources, links, news & events.


   http://climate-adapt.eea.europa.eu/
Why is water use a concern in Europe?
     Balance between demand and availability has reached a critical level in
      many areas of Europe (water scarcity)
     More and more areas are affected by weather changes, in particular less
      rain (droughts)
     Climate change will almost certainly make the situation worse
     More frequent and severe droughts expected across Europe and the
      neighbouring countries
     Total water abstraction in EU 247 billion m³/year:
       44% for energy production,
       24% for agriculture,
       17% for public water supply
     Agriculture is currently accountable for 85% of the global water
      consumption, and irrigated areas are expected to rise by a factor of 1.9 by
      2050, globally in the highest percentages where water-scarcity is most
      intense, namely South Europe Countries.
     For this reason, the need for improved water management practices, soil
      and crop, particularly in light of climate change, is growing.



Source: Martindale W., 2010. Food supply chain innovation. Aspects of Apll. Biol., 102, 1-6.
Climatic conditions in Europe – current status
                                                                      Over the past
                                                                      thirty years,
                                                                      droughts have
                                                                      dramatically
                                                                      increased in
                                                                      number and
                                                                      intensity in the
                                                                      EU, the number
                                                                      of areas and
                                                                      people affected
                                                                      by droughts
                                                                      increasing by
                                                                      almost 20%
                                                                      between 1976
Observed changes in annual precipitation between 1961-2006
                                                                      and 2006.

Source: EEA, Impacts of Europe's changing climate - 2008 indicator-
based assessment (2008).
Drought situation and related risks in CEE countries
         Slovenia                                    Romania                               Bulgaria                         Hungary




Agricultural drought in summer 2003            Areas affected by drought            Annual precipitation (mm)            Drought risk zones


                 Ukraine                                            Poland                                      Lithuania




       Crop yields in dry (2003) and non-dry            Spatial distribution of water deficit           Precipitation amount for May-July,
                    (2008) years                                    in 1992 year                                       2006


   Slovakia was affected by extreme droughts in several years: 2000, 2002, 2003, 2006,
   2007, 2008 and 2009). Also, the autumn of 2011 was the second driest since 1881.
Climatic conditions in Europe – projected changes
Drought is one of the most damaging natural hazards through its
effects on agricultural, hydrological, ecological and socio-economic
systems.
For the next two decades a warming of about 0.2°C per decade is
projected for a range of SRES emissions scenarios. Even if the concentrations
of all GHGs and aerosols had been kept constant at year 2000 levels, a further
warming of about 0.1°C per decade would be expected. Afterwards,
temperature projections increasingly depend on specific emissions scenarios.
 Drought prone areas and regions affected by heat waves are considered
likely to increase in extent. In Southern Europe especially climate change
is projected to worsen conditions (high temperatures and drought) in
a region that already faces water scarcity and heat waves in a
substantial number of areas. In Central and Eastern Europe, summer
precipitation is projected to decrease, causing higher water stress
(4-th Assessment Reports of the IPCC, 2007).

http://meetingorganizer.copernicus.org/EGU2012/EGU2012-563-2.pdf
http://ftp.jrc.es/EURdoc/JRC55386.pdf
Climatic conditions in Europe – projected changes

                                     In EUROPE, a mean
                                     annual air temperature
                                     increase of 2...4,5°C is
                                     foreseen by the end of
                                     the century, function of
                                     the scenarios of green
                                     house gas emissions.
                                     A 10...30% decrease of
                                     the annual precipitation
                                     amounts is estimated in
                                     the southern part of
                                     Europe, and even higher
                                     values in the north are
                                     expected.



(Source: IPCC, 4AR, 2007)
Climatic condition in Europe – projected changes
                                    Europe has seen an
                                    increase in temperature
                                    of 0.3°C per decade
                                    since the 1970s. At least
                                    two summers in the last
                                    decade (2003 and 2010)
                                    have been the warmest
                                    of the last 500 years in
                                    Europe. Southern Europe
                                    in particular is affected
                                    by hot summer days and
                                    tropical nights.
                                    Projections indicate an
                                    increase of the length,
                                    frequency and/or
                                    intensity of warm spells,
                                    or heat waves.


Source: EEA Report, No 2/2012
Climatic condition in Europe – projected changes
                                During the 20th century has been a
                                clear trend towards drier conditions,
                                with decreases in rainfall especially
                                in Southern and Eastern European
                                countries. The total area affected by
                                water scarcity and droughts
                                doubled - from 6 to 13 % - during
                                the last 30 years.
                                Future projections shows how the
                                precipitation deficit is projected to
                                change in the future in summer and
                                winter time. In this context, CC is
                                projected to lead to major changes
                                in water availability across Europe
                                with increasing water scarcity and
                                droughts mainly in Southern
                                Europe.


Source: EEA Report, No 2/2012
Climatic condition in Europe – projected changes
The water stress indicator (WEI) describes the ratio between total water withdrawals against water availability. It
  illustrates to which extent the total water demand puts pressure on the available water resources in a given
         territory and points out the territories that have high water demand compared to their resources.



                                                                            The results show that parts
                                                                            of southern and north-
                                                                            western Europe are already
                                                                            under severe water stress.
                                                                            Projected climatic changes
                                                                            shows that the situation
                                                                            worsens and most parts of
                                                                            Europe will be under severe
                                                                            or medium water stress.




 Source: EEA Report, No 2/2012
Potential impacts of CC on the status of water resources in drought
   conditions

In drought conditions climate change affects the following variables:
• water availability (river flows and groundwater levels)
         Annual river flow is projected to decrease in southern and south-eastern
         Europe and increase in northern Europe, but absolute changes remain uncertain.
         Climate change is projected to result in strong changes in the seasonality of river
         flows across Europe (EEA/JRC/WHO, 2008).
• water demand (esp. peak demands during periods of drought)
         Regions in southern Europe which already suffer most due to water stress are
         projected to be particularly vulnerable to reductions in water resources due to CC.
         In addition, higher temperatures are expected to lead to increased water demand,
         especially for irrigation and urban supply. This will result in increased competition for
         available resources (EEA/JRC/WHO, 2008).
• intensity and frequency of droughts
         The frequency and intensity of droughts are projected to increase in many regions of
         Europe, as a result of higher temperatures, decreased summer precipitation, and
         more and longer dry spells. The regions most prone to an increase in drought
         hazard are southern and south-eastern Europe (EEA/JRC/WHO, 2008).
What are the main sources of uncertainty on CC and drought impact ?

Uncertainties related on scientific information:
 Data availability, particularly with respect to the historical climatic series collected in the
  relevant database;
 The lack of common drought indicators – climatic, agricultural, hydrological, etc;
 The difficulties in modeling of drought impact based on climatic conditions and a
  variety of emission scenarios. The results are interpreted, described and published on a
  regular basis by the Intergovernmental Panel on Climate Change (IPCC);
 The spatial resolution of global models is insufficient for application in impact models
  and thereby for determining the effects of regional and local climate change. To overcome
  this limitation, regionalisation procedures are applied. By these, the global projections
  are “downscaled” to smaller grid elements of up to 25 km × 25 km. In individual studies the
  downscaling is even below this grid size, or adjusted to the locations of individual stations;
 Quantitative projections of changes in precipitation and the river flows at the river-
  basin scale are due to the limitations of climate models, as well as scaling issues between
  climate and hydrological models. Statistical correction methods have been developed
  which bring the models closer to a realistic simulation of, for instance, the amount and
  intensity of precipitation at the scale of river basins and small catchments.
Handling uncertainty

The handling related uncertainties of available scientific knowledge on CC and
drought:
In practical terms, decisions related to climate change impacts need to encompass several
adaptation options to the climate projections. In other words, decision makers will have to
handle and accept different options based on scenarios and be explicit about
uncertainty.
 A bottom-up approach in terms of looking at potential measures and considering how
each of these or combinations of them will perform against the range of possible climate
futures modeled.
Research and development projects can determine which sectors are impacted most
severely by climate change and where measures are needed most urgently to prevent
severe effects, even if their extent is not yet known.
Examples of information networks on DROUGHT
 At global level:
    - The World Meteorological Organization (WMO)
    - UNCCD Convention
    - The Global Water Partnership (GWP)
 in Europe:
- EC/DG Environment Program “Halting Desertification in Europe
- The United Nations Economic Commission for Europe (UNECE)
- The European Water Partnership (EWP)
- CLIMATE-ADAPT Platform
- ADAM Digital Compendium on Adaptation is a the portal for the dissemination of the trans-disciplinary
analysis results carried out in the EU ADAM project
- Research projects:
            - Research into climate change scenarios: PRUDENCE, ENSEMBLES, STARDEX,
           CECILIA, CLAVIER, CIRCA ERA-Net, CCWATERs, etc
           - Research on droughts and water scarcity: XEROCHORE, European Drought Observatory
           (EDO), WATERCoRe, MIDMURES, REDSIM, DESIRAS, I-ADAPT, Desert-net, DROUGHT-R&SPI;
           - Research into climate change impacts on the aquatic environment and water cycle: CLIME,
           KLIWAS, CLIMWATERADAPT, WATCH, CIRCE; WATER2ADAPT,
           - Research into mitigation / adaptation options and costs: AquaStress, ADAM, ClimateWater,
Drought management and adaptation options
The basic Framework to minimize the adverse impacts on the economy, social life
and environment when drought occurs, is the development of a specific Integrated
Drought Management Plan (IDMP).
Guiding principles:
1. Diagnose the causes that led to drought in the past and/or may lead to it in the future;
2. Monitor current drought conditions in order to detect water deficit early;
3. Develop a comprehensive set of indicators at appropriate temporal and spatial scale in
order to predict drought impacts;
4. Diagnose and improve knowledge of water deficit based on past and future trends,
incorporating climate change projections;
5. Analyze how predicted changes in mean annual rainfall will affect the socio-economic life
and environment;
6. Incorporate climate change adaptation in water management by continuing the focus on
sustainability (sustainable balance between water availability and demand).
7. Follow an integrated approach based on a combination of measures (compared to
alternatives based on water supply or economic instruments only);
8. Assess other climate change adaptation and mitigation measures on their impact on
drought risks.
IDMP initiative as a decisional tool

The outputs of IDMP initiative are:
          1. Knowledge base on recorded practices in drought planning and management;
          2. Guidance on tools and institutional arrangements to support increased risk responses;
          3. Advocacy through regional and country dialogues;
          4. Improved early drought warning services, building upon existing regional initiatives.

Recommendations in order to implement the outputs of IDMP initiative:
- to collaborate closely with WMO on the drafting the work plan on IDMP(2013-2015);
- to invite the DMCSEE and the European Drought Centre (EDO) to conduct the proposed activities and seek synergies;
- to invite and inform national secretariats of UNCCD of all CEE countries to contribute to specific case studies dealing with
degradation of land caused by desertification;
- to seek an appropriate mechanism and cooperation with agriculture sector at national levels;
- to invite the UNECE and its Task Force on Climate Change Adaptation to coordinate and share achievements in IDMP in CEE
region and seek a potential of the program replication in other signatory UNECE countries (specifically those in Central Asia,
where GWP has also its partners).
- to establish a web-based Integrated Drought Management Platform for:
                • commonly agreed products (e.g. objectively measurable drought indices covering as many contributing parameters
as possible);
                • joint comparison and analysis of information;
                • mutual exchange of knowledge & methodologies, and downscaling products;
                • real-time monitoring and forecasting products and services (early warning, preparedness).

     Policymakers need good information at the local, regional and European
    scales to identify priority issues, relevant sectors and economic activities.
Conclusions
     Climate change is likely to exacerbate current pressures on Europe's water
      resources. Increasingly, much of Europe will face reduced water availability
      especially during summer months, while the frequency and intensity of
      drought is projected to increase especially in the South. In the absence of
      sufficiently strong action, climate change may have also an sever impact
      on water management resources (EEA, 2010c).
     Environmental measures need to be implemented in the policies of all sectors
      affected by water scarcity and drought. To inform decisional makers at the
      regional and local levels the knowledge base for action needs to be improved.
      At the regional/local level it is crucial that competent authorities make any
      water management decisions in full awareness of the availability of water
      resources and in full awareness of the actual needs of all actors. Appropriate
      methodologies need to be implemented in order to provide effective monitoring
      and better management planning.


    Source: Towards efficient use of water resources in Europe, EEA Report No.1, 2012
Thank You!
elena.mateescu@meteoromania.ro
lipopesc@gmail.com

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Water Scarcity and Climate Uncertainty by Elena Mateescu, National Meteorological Administration, Romania and National Focal Point UNCCD

  • 1. 5 – 6 October 2012, Bratislava, Slovakia Integrated Drought Management Programme in Central and Eastern Europe A GWP and WMO initiative: Regional Workshop Agenda 5 October 2012 Drought management: current status and future regional perspectives, water management and agriculture sectors perspectives Water scarcity and climate uncertainty; what do we know on droughts in Europe Dr. Elena Mateescu - National Meteorological Administration, Romania Liviu Popescu – GWP, Romania
  • 2. Outline  Water scarcity and drought concepts  Water scarcity, drought and CC - policy framework  Knowledge base and information exchange on CC and drought – technical and scientific platform  Climatic conditions in Europe – current status and projected changes  Potential impacts of CC on the status of water resources in drought conditions  What are the main sources of uncertainty on CC and drought impact ?  Examples of information networks on DROUGHT  Drought management and adaptation options – IDMP  Conclusions
  • 3. Water scarcity and drought concepts Water scarcity is a man-made caused phenomenon. It is a recurrent imbalance that arises from an overuse of water resources, caused by consumption being significantly higher than the natural renewable availability. Water scarcity can be more aggravated by disturbed meteorological conditions during drought episodes and even more complicated by the water pollution which is associated with lack of resources (reducing the suitability for different water uses); Drought is a natural phenomenon. It is a temporary, negative and severe deviation along a significant time period and over a large region from average precipitation values (a rainfall deficit), which might lead to meteorological, agricultural, hydrological and socio-economic drought, depending on its severity and duration (EU definitions on WS&D Report, 2007). TIME SCALE Short-term Mid-term (months, Long-term (days, weeks) seasons, years) (decades) Causes Natural Dry spell Drought Aridity Man-made Water shortage Water scarcity Desertification Timescale and causes of water scarcity, drought and related concepts Source: Gap Analysis of the Water Scarcity and Droughts Policy in the EU, European Commission Tender ENV.D.1/SER/2010/0049 August 2012
  • 4. Water scarcity, drought and CC – policy framework Related on water scarcity and droughts policy, several EU policies and initiatives contribute to efforts for adaptation to climate change impact on water resources management; examples : EU Water Framework Directive (WFD/2000/60/EC) and the Water Scarcity and Droughts EU Policy (EC 2007b) refers : - to protect and restore the water environment across Europe by 2015 and to ensure the long term sustainable use of water; - to development of adaptation measures and sets out of a number of policy options for addressing impacts of water scarcity and droughts in next decades.  The Blueprint to safeguard Europe's water resources is a communication to be released by the end of 2012 that will address the evolution of water resources, including water's vulnerability to climate change and anthropogenic pressures (i.e. land use management). It will focus on different water resource management aspects that are related to adaption (land use management including forests, indicative water efficiency targets, economic instruments, innovation, governance and knowledge base). WATER SAVING SHOULD BECAME THE PRIORITY. Drought Management Plans must be the first set of policy options for future action
  • 5. Knowledge base and information exchange on CC and drought – technical and scientific platform The White Paper of the European Commission “Adapting to climate change: Towards a European framework for action” (COM/2009/147) issued in April 2009 sets out a framework to reduce the EU’s areas vulnerability to the water scarcity and drought. Starting with March 2012, the European Climate Adaptation Platform (CLIMATE- ADAPT) is a publicly accessible web-based platform designed to support policy-makers at EU, national, regional and local level in the development of climate change adaptation measures and policies;  The CLIMATE-ADAPT have been developed with the support of the European scientific and policy making community, and will help users to access, disseminate and integrate information on: - Expected climate change in Europe - The vulnerability of regions and sectors at present and in the future - National, regional and transnational adaptation activities and strategies - Case examples of adaptation and potential future adaptation options - Online tools that support adaptation planning - Adaptation-related research projects, guideline documents, reports information sources, links, news & events. http://climate-adapt.eea.europa.eu/
  • 6. Why is water use a concern in Europe?  Balance between demand and availability has reached a critical level in many areas of Europe (water scarcity)  More and more areas are affected by weather changes, in particular less rain (droughts)  Climate change will almost certainly make the situation worse  More frequent and severe droughts expected across Europe and the neighbouring countries  Total water abstraction in EU 247 billion m³/year:  44% for energy production,  24% for agriculture,  17% for public water supply  Agriculture is currently accountable for 85% of the global water consumption, and irrigated areas are expected to rise by a factor of 1.9 by 2050, globally in the highest percentages where water-scarcity is most intense, namely South Europe Countries.  For this reason, the need for improved water management practices, soil and crop, particularly in light of climate change, is growing. Source: Martindale W., 2010. Food supply chain innovation. Aspects of Apll. Biol., 102, 1-6.
  • 7. Climatic conditions in Europe – current status Over the past thirty years, droughts have dramatically increased in number and intensity in the EU, the number of areas and people affected by droughts increasing by almost 20% between 1976 Observed changes in annual precipitation between 1961-2006 and 2006. Source: EEA, Impacts of Europe's changing climate - 2008 indicator- based assessment (2008).
  • 8. Drought situation and related risks in CEE countries Slovenia Romania Bulgaria Hungary Agricultural drought in summer 2003 Areas affected by drought Annual precipitation (mm) Drought risk zones Ukraine Poland Lithuania Crop yields in dry (2003) and non-dry Spatial distribution of water deficit Precipitation amount for May-July, (2008) years in 1992 year 2006 Slovakia was affected by extreme droughts in several years: 2000, 2002, 2003, 2006, 2007, 2008 and 2009). Also, the autumn of 2011 was the second driest since 1881.
  • 9. Climatic conditions in Europe – projected changes Drought is one of the most damaging natural hazards through its effects on agricultural, hydrological, ecological and socio-economic systems. For the next two decades a warming of about 0.2°C per decade is projected for a range of SRES emissions scenarios. Even if the concentrations of all GHGs and aerosols had been kept constant at year 2000 levels, a further warming of about 0.1°C per decade would be expected. Afterwards, temperature projections increasingly depend on specific emissions scenarios.  Drought prone areas and regions affected by heat waves are considered likely to increase in extent. In Southern Europe especially climate change is projected to worsen conditions (high temperatures and drought) in a region that already faces water scarcity and heat waves in a substantial number of areas. In Central and Eastern Europe, summer precipitation is projected to decrease, causing higher water stress (4-th Assessment Reports of the IPCC, 2007). http://meetingorganizer.copernicus.org/EGU2012/EGU2012-563-2.pdf http://ftp.jrc.es/EURdoc/JRC55386.pdf
  • 10. Climatic conditions in Europe – projected changes In EUROPE, a mean annual air temperature increase of 2...4,5°C is foreseen by the end of the century, function of the scenarios of green house gas emissions. A 10...30% decrease of the annual precipitation amounts is estimated in the southern part of Europe, and even higher values in the north are expected. (Source: IPCC, 4AR, 2007)
  • 11. Climatic condition in Europe – projected changes Europe has seen an increase in temperature of 0.3°C per decade since the 1970s. At least two summers in the last decade (2003 and 2010) have been the warmest of the last 500 years in Europe. Southern Europe in particular is affected by hot summer days and tropical nights. Projections indicate an increase of the length, frequency and/or intensity of warm spells, or heat waves. Source: EEA Report, No 2/2012
  • 12. Climatic condition in Europe – projected changes During the 20th century has been a clear trend towards drier conditions, with decreases in rainfall especially in Southern and Eastern European countries. The total area affected by water scarcity and droughts doubled - from 6 to 13 % - during the last 30 years. Future projections shows how the precipitation deficit is projected to change in the future in summer and winter time. In this context, CC is projected to lead to major changes in water availability across Europe with increasing water scarcity and droughts mainly in Southern Europe. Source: EEA Report, No 2/2012
  • 13. Climatic condition in Europe – projected changes The water stress indicator (WEI) describes the ratio between total water withdrawals against water availability. It illustrates to which extent the total water demand puts pressure on the available water resources in a given territory and points out the territories that have high water demand compared to their resources. The results show that parts of southern and north- western Europe are already under severe water stress. Projected climatic changes shows that the situation worsens and most parts of Europe will be under severe or medium water stress. Source: EEA Report, No 2/2012
  • 14. Potential impacts of CC on the status of water resources in drought conditions In drought conditions climate change affects the following variables: • water availability (river flows and groundwater levels) Annual river flow is projected to decrease in southern and south-eastern Europe and increase in northern Europe, but absolute changes remain uncertain. Climate change is projected to result in strong changes in the seasonality of river flows across Europe (EEA/JRC/WHO, 2008). • water demand (esp. peak demands during periods of drought) Regions in southern Europe which already suffer most due to water stress are projected to be particularly vulnerable to reductions in water resources due to CC. In addition, higher temperatures are expected to lead to increased water demand, especially for irrigation and urban supply. This will result in increased competition for available resources (EEA/JRC/WHO, 2008). • intensity and frequency of droughts The frequency and intensity of droughts are projected to increase in many regions of Europe, as a result of higher temperatures, decreased summer precipitation, and more and longer dry spells. The regions most prone to an increase in drought hazard are southern and south-eastern Europe (EEA/JRC/WHO, 2008).
  • 15. What are the main sources of uncertainty on CC and drought impact ? Uncertainties related on scientific information:  Data availability, particularly with respect to the historical climatic series collected in the relevant database;  The lack of common drought indicators – climatic, agricultural, hydrological, etc;  The difficulties in modeling of drought impact based on climatic conditions and a variety of emission scenarios. The results are interpreted, described and published on a regular basis by the Intergovernmental Panel on Climate Change (IPCC);  The spatial resolution of global models is insufficient for application in impact models and thereby for determining the effects of regional and local climate change. To overcome this limitation, regionalisation procedures are applied. By these, the global projections are “downscaled” to smaller grid elements of up to 25 km × 25 km. In individual studies the downscaling is even below this grid size, or adjusted to the locations of individual stations;  Quantitative projections of changes in precipitation and the river flows at the river- basin scale are due to the limitations of climate models, as well as scaling issues between climate and hydrological models. Statistical correction methods have been developed which bring the models closer to a realistic simulation of, for instance, the amount and intensity of precipitation at the scale of river basins and small catchments.
  • 16. Handling uncertainty The handling related uncertainties of available scientific knowledge on CC and drought: In practical terms, decisions related to climate change impacts need to encompass several adaptation options to the climate projections. In other words, decision makers will have to handle and accept different options based on scenarios and be explicit about uncertainty.  A bottom-up approach in terms of looking at potential measures and considering how each of these or combinations of them will perform against the range of possible climate futures modeled. Research and development projects can determine which sectors are impacted most severely by climate change and where measures are needed most urgently to prevent severe effects, even if their extent is not yet known.
  • 17. Examples of information networks on DROUGHT  At global level: - The World Meteorological Organization (WMO) - UNCCD Convention - The Global Water Partnership (GWP)  in Europe: - EC/DG Environment Program “Halting Desertification in Europe - The United Nations Economic Commission for Europe (UNECE) - The European Water Partnership (EWP) - CLIMATE-ADAPT Platform - ADAM Digital Compendium on Adaptation is a the portal for the dissemination of the trans-disciplinary analysis results carried out in the EU ADAM project - Research projects: - Research into climate change scenarios: PRUDENCE, ENSEMBLES, STARDEX, CECILIA, CLAVIER, CIRCA ERA-Net, CCWATERs, etc - Research on droughts and water scarcity: XEROCHORE, European Drought Observatory (EDO), WATERCoRe, MIDMURES, REDSIM, DESIRAS, I-ADAPT, Desert-net, DROUGHT-R&SPI; - Research into climate change impacts on the aquatic environment and water cycle: CLIME, KLIWAS, CLIMWATERADAPT, WATCH, CIRCE; WATER2ADAPT, - Research into mitigation / adaptation options and costs: AquaStress, ADAM, ClimateWater,
  • 18. Drought management and adaptation options The basic Framework to minimize the adverse impacts on the economy, social life and environment when drought occurs, is the development of a specific Integrated Drought Management Plan (IDMP). Guiding principles: 1. Diagnose the causes that led to drought in the past and/or may lead to it in the future; 2. Monitor current drought conditions in order to detect water deficit early; 3. Develop a comprehensive set of indicators at appropriate temporal and spatial scale in order to predict drought impacts; 4. Diagnose and improve knowledge of water deficit based on past and future trends, incorporating climate change projections; 5. Analyze how predicted changes in mean annual rainfall will affect the socio-economic life and environment; 6. Incorporate climate change adaptation in water management by continuing the focus on sustainability (sustainable balance between water availability and demand). 7. Follow an integrated approach based on a combination of measures (compared to alternatives based on water supply or economic instruments only); 8. Assess other climate change adaptation and mitigation measures on their impact on drought risks.
  • 19. IDMP initiative as a decisional tool The outputs of IDMP initiative are: 1. Knowledge base on recorded practices in drought planning and management; 2. Guidance on tools and institutional arrangements to support increased risk responses; 3. Advocacy through regional and country dialogues; 4. Improved early drought warning services, building upon existing regional initiatives. Recommendations in order to implement the outputs of IDMP initiative: - to collaborate closely with WMO on the drafting the work plan on IDMP(2013-2015); - to invite the DMCSEE and the European Drought Centre (EDO) to conduct the proposed activities and seek synergies; - to invite and inform national secretariats of UNCCD of all CEE countries to contribute to specific case studies dealing with degradation of land caused by desertification; - to seek an appropriate mechanism and cooperation with agriculture sector at national levels; - to invite the UNECE and its Task Force on Climate Change Adaptation to coordinate and share achievements in IDMP in CEE region and seek a potential of the program replication in other signatory UNECE countries (specifically those in Central Asia, where GWP has also its partners). - to establish a web-based Integrated Drought Management Platform for: • commonly agreed products (e.g. objectively measurable drought indices covering as many contributing parameters as possible); • joint comparison and analysis of information; • mutual exchange of knowledge & methodologies, and downscaling products; • real-time monitoring and forecasting products and services (early warning, preparedness). Policymakers need good information at the local, regional and European scales to identify priority issues, relevant sectors and economic activities.
  • 20. Conclusions  Climate change is likely to exacerbate current pressures on Europe's water resources. Increasingly, much of Europe will face reduced water availability especially during summer months, while the frequency and intensity of drought is projected to increase especially in the South. In the absence of sufficiently strong action, climate change may have also an sever impact on water management resources (EEA, 2010c).  Environmental measures need to be implemented in the policies of all sectors affected by water scarcity and drought. To inform decisional makers at the regional and local levels the knowledge base for action needs to be improved. At the regional/local level it is crucial that competent authorities make any water management decisions in full awareness of the availability of water resources and in full awareness of the actual needs of all actors. Appropriate methodologies need to be implemented in order to provide effective monitoring and better management planning. Source: Towards efficient use of water resources in Europe, EEA Report No.1, 2012