Abstract
A high-resolution pre-industrial control simulation with the regional climate model REMO is analyzed in detail for different European subregions. To our knowledge, this is the first long pre-industrial control simulation by a regional climate model as well as at comparable resolution. We assess the ability of the climate model to reproduce the observed climate variability in various parts of the continent. In order to investigate the representation of extreme events in the model under pre-industrial greenhouse gas concentrations, selected seasons are examined with regard to the atmospheric circulation and other climatic characteristics that have contributed to the occurrences. A special focus is dedicated to land-atmosphere interactions. Extreme seasons are simulated by the model under various circumstances, some of them strongly resemble observed periods of extraordinary conditions like the summer 2003 or autumn 2006 in parts of Europe. The regional perspective turns out to be of importance when analyzing events that are constituted by meso-scale atmospheric dynamics. Moreover, the predictability of the European climate on seasonal to decadal time scales is examined by relating the statistics of surface variables to large-scale modes of variability impacting the North Atlantic sector like the Meridional Overturning Circulation, the El Niño Southern Oscillation, and the North Atlantic Oscillation. For this purpose, we introduce a measure of tail dependence that quantifies the correlation between extreme values in two variables that describe the state of the climate system. Significant dependence of extreme events can be detected in various situations.
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References
Alpert P, Baldini M, Ilani R, Krichak S, Price C, Rodo X, Saaroni H, Ziv B, Kishcha P, Barkan J, Mariotti A, Xoplaki E (2006) Relations between climate variability in the Mediterranean region and the tropics: ENSO, South Asian and African monsoons, hurricanes and Saharan dust. In: Lionello P, Malanotte-Rizzoli P, Boscolo R (eds) Mediterranean climate variability. Elsevier, Amsterdam
Belluci A, Gualdi S, Scicimarro E, Navarra A (2008) NAO-ocean circulation interactions in a coupled general circulation model. Clim Dyn. doi:10.1007/s00382-008-0408-4
Bengtsson L, Hodges KI, Röckner E, Brokopf R (2006) On the natural variability of the pre-industrial European climate. Clim Dyn 27:743–760. doi:10.1007/s00382-007-0168-y
Black E, Sutton R (2007) The influence of oceanic conditions on the hot European summer of 2003. Climate Dyn 28:53–66
Black E, Blackburn M, Harrison G, Hoskins B, Methven J (2004) Factors contributing to the summer 2003 European heatwave. Weather 59:217–223
Brönnimann S, Xoplaki E, Casty C, Pauling A, Luterbacher J (2007) ENSO influence on Europe during the last centuries. Clim Dyn 28:181–197
Carpenter G (2005) European flood report 2005–Central and Eastern Europe
Casty C, Raible CC, Stocker TF, Luterbacher J, Wanner H (2007) A European pattern climatology 1766–2000. Clim Dyn 11:11–11. doi:10.1007/s00382-007-0257-6
Cattiaux J, Vautard R, Yiou P (2009) Origins of the extremely warm European fall of 2006. Geophys Res Lett 36. doi:10.1029/2009GL037339
Chen D, Cane MA, Kaplan A, Zebiak SE, Huang D (2004) Predictability of El Niño over the past 148 years. Nature 428:733–736
Coelho CAS, Ferro CAT, Stephenson DB, Steinskog DJ (2008) Methods for exploring spatial variability of extreme events in climate data. J Clim 21:2072–2092
Coles S (2001) An introduction to statistical modeling of extreme values. Springer, New York
Coles S, Heffernan J, Tawn J (1999) Dependence measures for extreme value analyses. Extremes 2:339–365
Collins M, Botzet M, Carril AF, Drange H, Jouzeau A, Latif M, Masina S, Otteraa OH, Pohlmann H, Sorteberg A, Sutton R, Terray L (2006) Interannual to decadal climate predictability in the North Atlantic: a multimodel-ensemble study. J Clim 19:1195–1203
Czaja A, Frankignoul C (2002) Observed impact of Atlantic SST anomalies on the North Atlantic Oscillation. J Climate 15:606–623
D’Andrea F, Provenzale A, Vautard R, De Noblet-Decoudre N (2006) Hot and cool summers: Multiple equilibria of the continental water cycle. Geophys Res Lett 33. doi:10.1029/2006GL027972
Della-Marta PM, Luterbacher J, von Weissfluh H, Xoplaki E, Brunet M, Wanner H (2007) Summer heat waves over western Europe 1880–2003, their relationship to large scale forcings and predictability. Clim Dyn 29:251–275 doi:10.1007/s00382-007-0233-1
Dümenil L, Todini E (1992) A rainfall-runoff scheme for use in the Hamburg climate model. In: O’Kane J (ed) Advances in theoretical hydrology—a tribute to James Dooge. Elsevier, Amsterdam
Einmahl JHJ, de Haan L, Piterbarg VI (2001) Non-parametric estimation of the spectral measure of an extreme value distribution. Ann Stat 29:1401–1423
Feudale L, Shukla J (2007) Role of Mediterranean SST in enhancing the European heatwave of summer 2003. Geophys Res Lett 34. doi:10.1029/2006GL027991
Fink AH, Brücher T, Krüger A, Leckebusch GC, Pinto JG, Ulbrich U (2004) The 2003 European summer heatwaves and drought— synoptic diagnosis and impacts. Weather 59:209–216
Fischer EM, Schär C (2008) Future changes in daily summer temperature variability: driving processes and role for temperature extremes. Clim Dyn. doi:10.1007/s00382-008-0473-8
Fischer EM, Seneviratne SI, Vidale PL, Lüthi D, Schär C (2007) Soil moisture-atmosphere interactions during the 2003 European heat wave. J Clim 20:5081–5099
Fraedrich K, Müller K (1992) Climate anomalies in Europe associated with ENSO extremes. Int J Climatol 12(1):25–31
Hagemann S, Gates LD (2003) Improving a subgrid runoff parameterization scheme for climate models by the use of high resolution data derived from satellite observations. Clim Dyn 21:349–359
Hanson C, Palutikof J, Davies T (2004) Objective cyclone climatologies of the North Atlantic: a comparison af the ECMWF and NCEP reanalyses. Clim Dyn 22:757–769
Harvey LDD (2003) Characterizing and comparing control-run variability of eight coupled AOGCMs and of observations. Part 2: precipitation. Clim Dyn 21:647–658. doi:10.1007/s00382-003-0358-x
Harvey LDD, Wigley TML (2003) Characterizing and comparing control-run variability of eight coupled AOGCMs and of observations Part 1: temperature. Clim Dyn 21:619–646 doi:10.1007/s00382-003-0357-x
Haylock MR, Hofstra N, Tank AMGK, Klok EJ, Jones PD, New M (2008) A European daily high-resolution gridded data set of surface temperature and precipitation for 1950-2006. J Geophys Res 113. doi:10.1029/2008JD010201
Hirschi JJM (2007) Unusual North Atlantic temperature dipole during the winter 2006/2007. Weather 63:4–11
Hurrell JW (1995) Decadal trends in the North Atlantic Oscillation: regional temperatures and precipitation. Science 269:676–679
Jacob D (2001) A note to the simulation of the annual and inter-annual variability of the water budget over the Baltic sea drainage basin. Meteorol Atmos Phys 77(20):66–73
Jacob D, Göttel H, Jungclaus J, Muskulus M, Podzun R, Marotzke J (2005) Slowdown of the thermohaline circulation causes enhanced maritime climate influence and snow cover over Europe. Geophys Res Lett 32. doi:10.1029/2005GL023286
Jacob D, Bärring L, Christensen OB, Christensen JH, de Castro M, Déqué M, Giorgi F, Hagemann S, Hirschi M, Jones R, Kjellström E, Lenderink G, Rockel B, Sänchez E, Schär C, Sneviratne SI, Somot S, van Ulden A, van den Hurk B (2007) An inter-comparison of regional climate models for Europe: model performance in present-day climate. Clim Change 81:31–52
Jungclaus J, Haak H, Latif M, Mikolajewicz U (2005) Arctic-North Atlantic interactions and multidecadal variability of the meridional overturning circulation. J Clim 18:4013–4031
Jungclaus J, Botzet M, Haak H, Keenlyside N, Luo J, Marotzke J, Mikolajewicz U, Röckner E (2006) Ocean circulation and tropical variability in the coupled model ECHAM5/MPI-OM. J Climate 19:3952–3972
Keenlyside N, Latif M, Jungclaus J, Kornblueh L, Röckner E (2008) Advancing decadal-scale climate prediction in the North Atlantic sector. Nature 453:84–88
Latif M, Collins M, Pohlmann H, Keenlyside N (2006) A review of predictability studies of Atlantic sector climate on decadal time scales. J Clim 19
Lionello P, Bhend J, Buzzi A, Della-Marta PM, Krichak SO, Jansa A, Maheras P, Sanna A, Trigo IF, Trigo R (2006) Cyclones in the Mediterranean region: climatology and effects on the environment. In: Lionello P, Malanotte-Rizzoli P, Boscolo R (eds) Mediterranean climate variability. Elsevier, Amsterdam
Luterbacher J, Xoplaki E (2003) 500-year winter temperature and precipitation variability over the Mediterranean area and its connection to the large-scale atmospheric circulation. In: Bolle HJ (eds) Mediterranean Climate. Springer, Berlin
Luterbacher J, Liniger MA, Menzel A, Estrella N, Della-Marta PM, Pfister C, Rustishauser T, Xoplaki E (2007) Exceptional European warmth of autumn 2006 and winter 2007: Historical context, the underlying dynamics, and its phenological impacts. Geophys Res Lett 34. doi:10.1029/2007GL029951
Manabe S (1969) Climate and the ocean circulation 1: the atmospheric circulation and the hydrology of the earth’s surface. Mon Weather Rev 97:739–805
Mikosch T (2005) How to model multivariate extremes if one must. Statistica Neerlandica 59:324–338
Mitchell TD, Jones PD (2005) An improved method of constructing a data base of monthly climate observations and associated high-resolution grids. Int J Climatol 25:693–712
Müller WA, Röckner E (2008) ENSO teleconnections in projections of future climate in ECHAM5/MPI-OM. Clim Dyn. doi:10.1007/s00382-007-0357-3
Muskulus M, Jacob D (2005) Tracking cyclones in regional model data: the future of Mediterranean storms. Adv Geosci 2:13–19
Ogi M, Yamazaki K, Tachibana Y (2004) The summer northern annular mode and abnormal summer weather in 2003. Geophys Res Lett 32
Olea RA, Pawlowski-Glahn V (2009) Kolmogorov-Smirnov test for spatially correlated data. Stoch Environ Res Risk Ass 23:749–757
Pohlmann H, Sienz F, Latif M (2006) Influence of the multidecadal Atlantic meridional overturning circulation variability on European climate. J Clim 19:6062–6067
Pohlmann H, Jungclaus J, Köhl A, Stammer D, Marotzke J (2009) Initializing decadal climate predictions with the GECCO oceanic synthesis: effects on the North Atlantic. J Clim 22:3926–3938
Röckner E, Bauml G, Bonaventura L, Brokopf R, Esch M, Giorgetta M, Hagemann S, Kirchner I, Kornblueh L, Manzini E, Rhodin A, Schlese U, Schulzweida U, Tompkins A (2003) The atmospheric general circulation model ECHAM5. Part I: model description. In: MPI Report 349, Max Planck Institute for Meteorology, Hamburg
Schär C, Vasilina L, Pertziger F, Dirren S (2004a) Seasonal runoff forecasting using model-assimilated precipitation data. J Hydrometeorol 5:959–973
Schär C, Vidale PL, Lüthi D, Frei C, Häberli C, Liniger MA, Appenzeller C (2004b) The role of increasing temperature variability in European summer heatwaves. Nature 427:332–336
Sillmann J, Croci-Maspoli M (2008) Atmospheric blocking and extreme events in the present and future climate. Geophys. Res. Lett.
Trigo IF, Bigg GR, Davies TD (2002) Climatology of cyclogenesis mechanisms in the Mediterranean. Mon Weath Rev 130:549–569
Trigo R, Xoplake E, Zorita E, Luterbacher J, Krichak SO, Albert P, Jacobeit J, Saenz J, Fernandez J, Gonzalez-Rouco F, Garcia-Herrera R, Rodo X, Brunetti M, Nanni T, Maugeri M, Turkes M, Gimeno L, Ribero P, Brunet M, Trigo IF, Crepon M, Mariotti A (2006) Relations between variability in the Mediterranean region and mid-latitude variability. In: Lionello P, Malanotte-Rizzoli P, Boscolo R (eds) Mediterranean climate variability. Elsevier, Amsterdam
Trigo RM, Garcia-Herrera R, Diaz J, Trigo IF (2005) How exceptional was the early August 2003 heatwave in France? Geophys Res Lett 32. doi:10.1029/2005GL022410
Ulbrich U, Brücher T, Fink AH, Leckebusch GC, Krüger A, Pinto JG (2003) The Central European floods of August 2002: Part 1 – rainfall periods and flood developement. Weather 58:371–391
van den Hurk B, Haarsma R, Selten F, Seneviratne S (2009) Soil drying in Europe and its impact on atmospheric circulations. In: Proc ECMWF semin parametrizations subgrid phys process
van Oldenborgh GJ (2007) How unusual was autumn 2006 in Europe. Clim Past 3:659–668
Yiou P, Vautard P, Naveau P, Cassou C (2007) Inconsistency between the atmospheric dynamics and temperature during the exceptional 2006/2007 fall/winter and recent warming in Europe. Geophys Res Lett 34. doi:10.1029/2007GL031981
Zhang Z (2008) Quotient correlation: a sample based alternative to Pearson’s correlation. Ann Stat 36:1007–1030
Zaitchik BF, Macalady AK, Bonneau LR, Smith RB (2006) Europe’s 2003 heatwave: a satellite view of impacts and land atmosphere feedbacks. Int J Climatol 26
Zappa M, Rotach MW, Arpagaus M, Dorninger M, Hegg C, Montani A, Ranzi R, Ament F, Germann U, Grossi G, Jaun S, Rossa A, Vogt S, Walser A, Werhan J, Wunram C (2008) MAP D-PHASE: real-time demonstration of a hydrological ensemble prediction system. Atm Science Lett 9:80–87
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We would like to thank Bjorn Stevens, Monika Esch, Michael Botzet, Wolfgang Müller, Johann Jungclaus, Philip Lorenz and Alberto Elizalde for support and helpful discussions.
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Appendix Atmospheric characteristics of extreme events
Appendix Atmospheric characteristics of extreme events
In the following we describe the atmospheric characteristics of the extreme events referred to in Sect. 3.
1.1 Temperature extremes
1.1.1 Summer 2434
Very high temperatures occur in Central Europe, but also in the Alps, France, the Mediterranean, Eastern Europe, and on the Iberian Peninsula. A high-pressure system is centered over Central Europe, a low-pressure through North East of Scandinavia. Seasonal mean winds are from the South West to the Iberian Peninsula, the Alps, and Central Europe.
For Central Europe, the Alps, France, and the Iberian Peninsula highest temperatures take place in July. The high-pressure system over Central Europe remains stagnant over the season. The pressure gradients get somewhat flatter in August and the core of the high is moving slightly to the East. Accordingly, highest temperatures for Eastern Europe and the Mediterranean occur in August.
Negative cloud cover anomalies are obvious all over the continent except Scandinavia. The main signal covers Central Europe, the Alps, France, the Mediterranean, and Eastern Europe. Incoming solar radiation and surface thermal radiation anomalies match broadly with cloud cover anomalies. Latent heat flux anomalies are positive over the season in Central Europe, France, the Iberian Peninsula and most of Scandinavia, but negative in parts of the Mediterranean and Eastern Europe, indicating a drying of the soil in these areas.
1.1.2 Autumn 2351
Especially warm conditions prevail on the British Islands, but high temperatures are attained also in the Alps, Central Europe, France, and Scandinavia. The high-pressure system centered over the southern Baltic Sea attracts warm air from the South to the British Islands, the Alps, and Central Europe. Low pressure establishes itself over Iceland. Eastern Europe experiences winds from the North.
In all regions, temperatures are highest in September and lowest in November, but extraordinary warm conditions prevail also in October. In September the high is centered over Scandinavia, extending to the British Islands, Central Europe, the Mediterranean, and Eastern Europe, bringing warm air on the western side to the British Islands and Central Europe. In October and November the atmospheric condition is very stable.
The negative cloud cover anomaly over the British Islands is not particularly pronounced suggesting that the anomalously high temperatures are mainly due to the advection of southerly warm air. Latent heat flux anomalies are positive in parts of the British Islands, France, and the Iberian Peninsula, but negative values dominate on the rest of the continent.
1.1.3 Spring 2257
Very warm conditions dominate in the Mediterranean, but also on the Iberian Peninsula, in Eastern Europe, and the Alps, to a lesser extent in France, Central Europe, and Scandinavia. High pressure extends over Eastern Europe, and the wind transports warm air from the South to the Alps and the Mediterranean.
High temperatures already affect the Mediterranean and the Alps in April, but the warming even increases in May. The atmospheric state is not extraordinarily stable. In March a high-pressure system is located over Central Europe, moving to the Mediterranean in April. A low establishes west of the European continent in May, high pressure extends from Iceland to Eastern Europe, causing southerly airflow to the Mediterranean. The reasons for warm temperatures in the Mediterranean are different in April and May. The advection of warm air from the south plays an important role, the very warm spring in the Mediterranean is a dynamical phenomenon rather than provoked by stable conditions.
Less cloud cover than average can be asserted mainly in the Mediterranean and Eastern Europe. The distinct negative latent heat flux anomalies are primarily restricted to the Mediterranean and the Iberian Peninsula.
1.1.4 Summer 2180
Extraordinary high summer temperatures strike Eastern Europe, very warm conditions also prevail in Central Europe, the Alps, France, and the Mediterranean. A very strong and persistent high-pressure system remains stable and centered over Eastern Europe, covering the whole continent. Winds from the North West keep temperatures moderate on the British Islands.
The Alps and Central Europe experience warmest temperatures in July, Eastern Europe and the Mediterranean in August. Strong high pressure with centre over France can be observed in June (when France experiences highest temperatures), moving to the East in July. Warm air from the south is transported to the Mediterranean. The high is moving further east in August, when a low-pressure system develops northwest of the British Islands. The atmospheric circulation shows little variation, especially in Eastern Europe and the Mediterranean, where a strong blocking pattern prevails.
Very distinct negative cloud cover anomalies extend all over Europe, with the exception of Scandinavia and the British Islands. Strongest anomalies affect Eastern Europe, where the heat wave is most pronounced. Latent heat flux anomalies are negative in the Mediterranean, Eastern Europe, Central Europe, and Scandinavia, positive on the Iberian Peninsula, parts of France and the British Islands.
1.2 Precipitation extremes
1.2.1 Autumn 2228
Very high precipitation occurs in the Alps and the Iberian Peninsula, but also in France, the Mediterranean, and Eastern Europe. A strong cyclone is centered over the Alps, while Scandinavia and the British Islands are on the edge of this low-pressure system. Westerly airflow dominates over the continent.
In the Alps and France strongest precipitations fall in September, least in October. On the Iberian Peninsula rainfall increases over the three autumn months. Eastern Europe sees strongest precipitation in October. The low-pressure system remains stable over the Alps. It is less extended in September, somewhat weaker in October, but stretching more to the East.
Positive cloud cover anomalies cover the Alps, France, the Iberian Peninsula, the Mediterranean, and Eastern Europe. Latent heat fluxes are above average over most of Europe except on the British Islands and parts of Central Europe and Scandinavia.
1.2.2 Winter 2362
Very high precipitation anomalies affect France, but also Central Europe, and the Alps. An extended low-pressure system is centered over Europe with westerly flow conditions.
For France, Central Europe, and the Alps strongest precipitations occur in January, but rainfall is distinctly above average also in December. Pressure conditions are very stationary over the three months. Westerly windflow impacts the three regions with highest precipitation anomalies.
Positive cloud cover anomalies can be observed in a band from the Iberian Peninsula to France, Central Europe, and the Alps, correlating clearly with the precipitation anomalies. Correspondingly, a strong positive anomaly in latent heat fluxes affects France and the regions of high rainfall.
1.2.3 Spring 2343
The British Islands receive an anomalous amount of precipitation, but the rainfall is high also in Scandinavia. In the Mediterranean the amount of precipitation is below average. The low-pressure belt extends from North West of the British Islands, over the British Islands and towards Scandinavia. The cyclonic structure of the flow leads to west winds over the British Islands.
On the British Islands and Scandinavia highest precipitation falls in March. The pressure system is not particularly stable. In March the atmospheric state is similar to the seasonal mean situation. In May, a low-pressure ridge extends from the British Islands southeastwards to Eastern Europe, while high pressure is located over Scandinavia. In April a low-pressure band stretches over Northern Europe. From the continental point of view, the situation is quite dynamic, but the British Islands remain influenced by northeasterly airflow and low-pressure conditions throughout the season.
Positive cloud cover anomalies reside over the British Islands, Southern Scandinavia, and Northern Central Europe. A positive signal in latent heat fluxes can be observed on the British Islands, in the Alps, and parts of Scandinavia.
1.2.4 Winter 2317
Very high precipitation can be observed in the Mediterranean, rather low in Central Europe, British Islands, and Scandinavia. A strong low-pressure system remains stationary over the whole season in the Mediterranean, and high pressure over Scandinavia. A cyclonic structure of the wind can be observed over the Mediterranean. The NAO is in a distinct negative phase.
Precipitation over the Mediterranean is highest in January, but strong also in December. According to the pressure pattern, cloud cover anomalies restrict mainly to the Mediterranean. No distinct signal is apparent in other regions. Latent heat flux anomalies are strongly positive over almost the whole Mediterranean Sea, but negative over the British Islands and Central Europe.
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Tomassini, L., Hagemann, S., Moseley, C. et al. Extremes and predictability in the European pre-industrial climate of a regional climate model. Clim Dyn 36, 2371–2397 (2011). https://doi.org/10.1007/s00382-010-0814-2
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DOI: https://doi.org/10.1007/s00382-010-0814-2