Climate Change and the European Water Dimension - Agri ...

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Climate Change and the European Wat
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European Commission- Joint Research
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At the 2003 Rome Informal Meeting o
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Changes in the diurnal variation of
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Fugure I.2. (a) Maximum grid covera
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century. This corresponds to a sea
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Other causes Other causes of climat
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tropospheric ozone are photochemica
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Figure. I.4. Radiative forcings and
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There are two indirect effects of a
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The projected warming is not unifor
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water towards the west Pacific caus
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Aerosols and climate change in the
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precipitation intensities have been
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Chapter III. The Hydrologic Cycle I
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Figure III.2. Long-term average ann
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Figure III.4. Projected change in s
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eduction in the rate of evaporation
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characteristics may or may not be u
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temperatures potentially lead to hi
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Chapter IV.A. Proxy indicators of C
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Mean Air Temperature (Dec.-March) [
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correlation coefficient -0.4 -0.3 -
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Chapter IV. B. The Impact of Climat
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numbers refer to water bodies bigge
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Table IV.B.2. Number of large dams*
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quality degradation and meet the in
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sufficient resolution and accuracy
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Windermere in the English Lake Dist
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their vertical structure. In partic
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have recently described a method th
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The available evidence suggests tha
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1979). In contrast, heavy rain incr
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The projected increase in the atmos
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Aulacoseira spp. favour the changed
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vertical bars are a simple measure
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values, with an upper limit of 30°
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the processes controlling, regional
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Sea level rise is partially due to
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Box # 1: The North Sea The North Se
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and organic material more rapidly t
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suggesting that climate rather than
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CO2 2- ). In turn, the alkalinity i
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looms are often associated with tox
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events of dense water through the D
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(1) Are we already observing a resp
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eastern and western side of the Nor
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system, their physiology and intern
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each coastal element be studied and
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IV.D.1. Introduction Coastal lagoon
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In the last decade, a general model
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topics in coastal lagoons (de Wit e
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Po River Delta lagoons, the long dr
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esilient to environmental changes a
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Chapter V.A. Climate Change and Ext
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It is realized that adaptation to c
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member states. Moreover some agenci
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Large, global scale climatic driver
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V.B.5. Climate change and droughts
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Evacuation from forest fires at Mas
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In European forest policy, water is
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Drought mitigation and the involvem
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DSS-DROUGHT A Decision Support Syst
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Chapter V .C. Climate Change, Ecolo
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The quality class boundaries within
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An example of this kind of relation
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Regions 1 to 5 represent mainly a m
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een observed in southwestern countr
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Table V.D.2: Percentage area affect
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Lake Surface Temperature [°C] Desc
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Case Study: Esthwaite Water, Cumbri
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Residence time (days) Chlorophyll (
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Case Study: Lake Erken, Sweden ►
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TP (µg l -1 ) Modelling To analyse
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Data availability and investigation
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smaller volume of water. The warmer
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Chapter VI.B. Climate Change and th
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Concerning the flora of the lagoon
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Figure VI.B.2: Frequency of “bora
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Figure VI.C.2. Daily flows in Ebro
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Figure VI.C.4. Mean temperature inc
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Page 199 and 200: severe flooding were investigated (
Page 201 and 202: Table VI.E.1. Waterborne pathogens
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Page 205 and 206: Areas behind the dikes broken in 20
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Page 215 and 216: Table VI.F.1. Priority substances i
Page 219 and 220: 22. Monteith, J.L., 1965. Evaporati
Page 221 and 222: 31. Rodionov, S.N. 1994. Global and
Page 223 and 224: 28. Dokulil, M.T., 2003. Algae as e
Page 225 and 226: 63. Hejzlar, J., Dubrovský, M. Buc
Page 227 and 228: 99. Melack, J.M., J. Dozier, C.R. G
Page 229: 136. Straile, D. & Adrian, R. 2000.
Page 233 and 234: 60. McCleery, R. H. and Perrins, C.
Page 235 and 236: 105. UNESCO 2003. The integrated st
Page 237 and 238: ecosystems and the landscape and de
Page 239 and 240: 2. Carter, T.R., Saarikko, R.A., an
Page 241 and 242: 24. Hydrographisches Zentralbüro 1
Page 243 and 244: European Coastal Lagoons: The Influ
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Page 251 and 252: France GIANMARCO GIORDANI Departmen
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