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Impacts of climate change on regions: European territory of Russia

Impacts of climate change on regions: European territory of Russia. Anatoly Shvidenko on behalf of the authors of Chapter 12 of the WG II Contribution to the 4 th AR of the IPCC. Europe and European Russia in a global picture.

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Impacts of climate change on regions: European territory of Russia

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  1. Impacts of climate change onregions: European territory of Russia Anatoly Shvidenko on behalf of the authors of Chapter 12 of the WG II Contribution to the 4th AR of the IPCC

  2. Europe and European Russia in a global picture Multi-model projected patterns of precipitation change 2090-2099 to 1980-1999, SRES A1B, WGI Figure 10.9

  3. Climate change 2007: Synthesis Report

  4. Regional specifics and heterogeneity • On average, major regularities of global climate change over Northern Hemisphere are also observed in Europe and European Russia • However, there are distinct regional features of climate change within the region and its parts; it generates diverse impacts, different positive and negative consequences and feedbacks, as well as needs of regional adaptation and mitigation measures taking into account current and expected socio-economic condition and the demographic trends

  5. Climate change in European Russia Regional trends of annual average air temperature In 1970-2004 by regions of European Russia and empirical forecast by 2025 Region 1 2 3 4 5 6 Trend (oC/10 y) 0.2 0.3 0.3 0.3 0.2 0.3 Forecast - 0-0.5 0-0.5 - - 0.2-0.5 Correlation coefficients between global and regional air temperature in 1900-2004 (R), first (R1) and second (R2) half of 20th century by regions Region 1 2 3 4 5 6 R 0.42 0.59 0.70 0.66 0.69 0.76 R1 0.44 0.11 0.24 0.06 0.05 0.11 R2 0.53 0.81 0.85 0.76 0.70 0.83 Source: Anisimov et al. 2007

  6. Relative runoff changes

  7. Projections of climate, cryosphere, and terrestrial ecosystems Modeled mean annual temperature at the permafrost surfacein Northern Eurasia (Romanovsky et al. 2007). 1980-2000 2080-2100 Dynamics of permafrost as follows from INM RAS climate model experiments: in 1981-2000 (top), 2081 - 2100 under scenario В1 (middle) and in 2081 - 2100 under scenario А2 (bottom)(Lykosov et al. 2007)

  8. Land cover feedback in north:Two possible scenarios of land cover change after the permafrost thaw and it began thaw: Wetlands Steppe

  9. Increasing climate variability and extreme weather events at different temporal and spatial scales: expected frequency and severity of heat waves; numbers of days with heavy precipitation etc. Summer (June to mid-August) 2003 heat wave: JJA temperature anomaly of 3 to 5oC in most southern and Central Europe

  10. Changes in the surface water cycle over Northern Eurasia that have been statistically significant in the 20th century Regions with more humid conditions (blue), regions where potential forest fire danger has increased in the 20th century (red),the region where agricultural droughts have increased (circled), andthe region where prolonged dry episodes have increased (rectangled). Major wheat producing area in Northern Asia Mescherskaya &Blazhevich (1997 updated), Dai et al. (2004), Zhai et al. (2005), Niu and Zhai (2008), Groisman et al. (2005, 2007), Groisman and Knight (2007)

  11. Main expected impacts of climate change in Europe during the 21st century, assuming no adaptation

  12. Main expected impacts of CC in Europe during the 21st century, assuming no adaptation

  13. Key vulnerabilities

  14. Global change impacts productivity and biogeochemical cycling of forests Major drivers impacted productivity of forests climate change • climate change • CO2 fertilization effect • nitrogen deposition • disturbance (fire and insects) • forest management Live biomass NPP Empirical estimate of NPP 297 g C m-2yr-1 Average NPP of 17 DGVMs 338 g C m-2yr-1 (Shvidenko et al. 2008) Empirical estimate of increasing productivity on average + 0.5% per year during 1960s-2005 (Alexeyev & Markov 2003; Shvidenko et al.2007)

  15. Statistically significant change of structure of live biomass of Russian forests in 1960-2005 Dynamics of ratio of LB to growing stock (red-stem wood, blue-roots, green-foliage) (average data of 3745 sample plots) Dynamics of the ratio for all Russian forests (normalized to the values of 1983)

  16. Increasing risk of disturbances Three major drivers of accelerating disturbances in forests: variability of climate, anthropogenic factors and insufficient governance Fire, insects, windbreaks, combined impacts

  17. DISTURBANCES:Vegetation & Forest Fires in Russia 2003(integrated multi-sensor remote sensing data) During last 10 years area of vegetation fire (above 2/3 – on forest land) exeeded 10 million ha 9

  18. DYNAMICS OF FIRES NUMBERS AND BURNED AREA (PROTECTED TERRITORY OF RUSSIA) Korovin and Zukkert 2003, updated

  19. Carbon Fluxes (Tg C) due to disturbance in Russian forests in 1960-2005

  20. Key uncertainties and research needs • Improved long-term monitoring of climate-sensitive sectors and systems; development of integrated observing systems • Improvement of climate impact models, development of regional models • Enhancement of climate change impact assessment in areas with little or no previous investigation • Understanding of terrestrial biota functioning under multiple stress • Development of integrated impact models – needs of the corresponding studies with a special emphasis to human dimension and socio-economic aspects

  21. Adaptation & mitigation measures • The comprehensive evaluation of adaptation and mitigation measures and technologies used in different regions of Europe to reduce the adverse impact of climate variability and extreme meteorological events • Better understanding, identification and prioritisation of adaptation options in agriculture, aquatic ecosystems, forest management, health services etc. • Evaluation of the feasibility, costs and benefits of potential adaptation options, measures and technologies • Quantification of bio-climatic limitations of most important plant species • Intensification of studies on the regional specifics of adaptive capacity

  22. Implementation • Identification of populations at risk and the lag of climate change impacts • Approaches for including climate change in management policy and institutions • Consideration of non-stationary climate in the design of engineering structures • Identification of the implications of climate change for water, air, health and environmental standards • Identification of the pragmatic information needs of managers responsible for adaptation

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