Fig. 7.33. Seasonal anomalies, with respect to the 1961-90 mean, of sea level pressure (hPa) from NCAR/NCEPreanalyses. Colored shading represents the percentageof accumulated seasonal precipitation compared withthe 1951–2000 climatology from the seasonal GPCCprecipitation data set (only values above 15 mm perseason are represented). Thick black lines highlightthose sea level pressure anomalies which are greaterthan one standard deviation above the mean.and western Russia, where temperature anomaliesexceeded +3°C. Increased cyclonicity led to wellabove-averageNovember precipitation, particularlyin the northern half of Europe with new records setacross Ireland and the UK.The end of the year was characterized by an extremelynegative phase of the Arctic Oscillation (AO)with high pressures dominating the higher latitudesof the Northern Hemisphere, affecting the weatherin Europe. The AO Index in December <strong>2009</strong> was-3.4, the lowest value observed for thatmonth in 60 years (Fig. 2.30b in Section2d), with extremely negative values in thesecond half of the month. Most of Europewas under the influence of a stronghigh pressure system over the Arcticand Scandinavia that favored intenseadvection of cold polar air far into themiddle latitudes (Trigo et al. 2004). Thenegative North American Oscillationindex in December also contributed toa starkly contrasting temperature patternover Europe. While SoutheasternEurope and parts of the polar region(Greenland, Iceland, Svalbard) experiencedmild temperatures—GreenlandS162 | juNE 2010was 7°C warmer than average—colder-than-averageconditions prevailed over the northern half of Europewith heavy snowfall in places. The Scandinavian highpressure also caused a dry December in NorthernEurope, while most of the rest of Europe, particularlythe South, experienced a very wet end of the year.2) Central and Western Europe—A. Obregón, P. Bissolli,J. J. Kennedy, and D.E. ParkerCountries considered in this section include: Ireland,the United Kingdom, the Netherlands, Belgium,Luxembourg, France, Germany, Switzerland, Austria,Poland, Czech Republic, Slovakia, and Hungary.(i) TemperatureAnnual mean temperatures in Central Europewere 1°C–2°C above the 1961–90 average throughoutmost of the region (Fig. 7.29). Over Western Europe,anomalies were mostly below +1°C.Winter 2008/09 was the coldest in the UK since1996/97. In France, it was the third coldest winter in20 years. Severe cold waves during January and Februarybrought temperatures below -25°C to Germanyand Poland. The lowest recorded daily minimumtemperature in <strong>2009</strong> in Poland was -28.2°C in thesouthwest of the country on 7 January. A privateweather service station in Saxony, eastern Germany,recorded -29.1°C on the same day. In contrast, winterwas warmer than average in the easternmost regions(Poland, Czech Republic, Slovakia, Austria, andHungary; Fig. 7.32a).Spring temperatures were well above average,mainly due to an exceptionally warm April (Fig. 7.34).Belgium and Switzerland each reported their secondwarmest spring on record. April was the secondwarmest on record for De Bilt in the NetherlandsFig. 7.34.Monthly mean anomalies of surface air temperature acrossEurope and over the North Atlantic, April <strong>2009</strong> (1961–90 base period)based on CLIMAT and ship observations. [Source: DeutscherWetterdienst (DWD).]
(1706–<strong>2009</strong>), and new national records were set formean anomalies in Hungary (+4.2°C) and Germany(+4.5°C; 1901–<strong>2009</strong>).Summer temperatures were generally above average(Fig. 7.32c), most notably in southern France andSwitzerland where anomalies were more than +2°C. Asignificant heat wave affected Western Europe duringJuly, while a heat wave in France from 15–20 Augustresulted in temperatures above 36°C in the North and40°C in the South.Monthly mean temperatures for November wereamong the three warmest in the last century acrossthe United Kingdom, Netherlands, Belgium, France,and Germany. In southern Germany, maximumtemperatures of around 20°C were reached as a resultof foehn winds; such high temperatures are unusualduring November.December was cold especially in the UK andIreland but also in northern Central Europe and onboth sides of the Alps, with anomalies below -1°C.This was mainly due to a long cold spell in the secondhalf of the month.(ii) PrecipitationAnnual precipitation amounts were normal orabove normal in Central Europe (Fig. 7.30), thoughsome regions in southern France received only 70–80% of their normal totals. The United Kingdom andIreland experienced a wet year. Valentia Observatoryin Ireland reported its highest annual rainfall totalsince records began in 1866.Winter was mainly dry throughout Central andWestern Europe (around 60%–80% of normal, Fig.7.33, DJF), but with heavy snowfall in some areasparticularly during February. In February and March,heavy snowfall in parts of the northern Alpine regionresulted in peak snow depths of over four meters.It was the driest spring since 1997 in England andWales, while March was exceptionally wet in easternCentral Europe; the Czech Republic reported almostdouble its average March rainfall. April was very dryin eastern Central Europe. Hungary recorded only23% of its average 1971–2000 April rainfall, whilePoland experienced rainfall in the 10th percentile ofits 1961–90 distribution.England and Wales had their wettest July onrecord, while western Scotland had its wettest Augustsince records began in 1910. This was the thirdconsecutive wet summer in the UK and Ireland (Fig.33, JJA). In Switzerland, the city of Lugano reportedits highest July precipitation (397 mm) since recordsbegan in 1864, mainly due to two large thunderstormsduring the middle of the month. In contrast, dryconditions in August and September prevailed overWestern and Central Europe.November was the wettest in recorded historyacross the UK and most of Ireland. The Alps hadreceived intense snowfalls by the end of November.December again was a wet month in most of Westernand Central Europe but very dry in Ireland andScotland.(iii) Notable eventsA severe North Atlantic storm with strong windsup to 174 km hr -1 affected the UK and Ireland on17 January. Another Atlantic storm, with gusts ofhurricane force, affected Western Europe on 23–24January. Southern Ireland saw heavy rain with severeflooding on 29–30 January.Unusual snow events affected Western Europe atthe beginning of the year. On 6–7 January, a Mediterraneanstorm dropped 20 cm–40 cm of snow acrosssoutheastern France for the first time since 1987.At the beginning of February, the United Kingdomexperienced its most widespread snowfalls since1991, resulting in peak snow depths of up to 30 cm.London received its heaviest snowfalls in 18 years. Inthe Alpine region, the snows lasted until the end ofFebruary even at low elevations, which was unusual,especially south of the Alps.Various episodes of heavy rainfall occurred duringsummer. On 6 June and 16–17 July, the UnitedKingdom experienced daily totals of more than 90mm. Likewise, heavy precipitation, flooding, andmudslides affected Central Europe on 21 June. On 2July, Dublin was affected by flooding after torrentialrainfall. A severe storm on 23 July affected Germany,Poland, and the Czech Republic.Autumn also had some noteworthy heavy rainevents with flooding. On 3 September in northeastScotland, daily totals exceeded 120 mm. Parts ofAberdeen city centre were flooded with disruptionsto roads and rail services. A frontal system movingacross the Atlantic Ocean caused record precipitationand widespread flooding in northwestern England on18–20 November (see sidebar). Central Europe experiencedgusts of hurricane force on 23–24 November.A severe cold spell and heavy snowfall 15–22December affected most of the region. Temperaturesbelow -20°C were reported in Germany and France.The Netherlands experienced unusually heavy snowfall,with snow depths up to 30 cm. Cold and snowyconditions continued into 2010.<strong>STATE</strong> <strong>OF</strong> <strong>THE</strong> <strong>CLIMATE</strong> <strong>IN</strong> <strong>2009</strong> juNE 2010 |S163
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Luo, Jing-Jia, Research Institute f
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Tedesco, Marco, Department Earth an
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4. THE TROPICS.....................
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ABSTRACT—M. O. Baringer, D. S. Ar
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I. INTRODUCTION—M. O. Baringer an
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Table 1.1 The GCOS Essential Climat
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S18 | juNE 2010
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Stratospheric TemperatureCloudiness
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Source Datasets Sectionhttp://www.p
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HOW do WE KNOW THE WORLD HAS WARMED
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Fig. 2.6. As for Fig. 2.1 but for l
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Fig. 2.10. Change in TCWV from 2008
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Precipitation anomalies in 2009, ov
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Fig. 2.18. Seasonal SCE anomalies (
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USING SI-TRACABLE GLOBAL POSITIONIN
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6) Lake levels—C. BirkettLake vol
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Fig. 2.30. (a) The daily AO index f
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(C) Carbon monoxide (CO)There has b
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Table 2.5. Mixing ratios, radiative
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the mid-1990s but has since levelle
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with all 42 glaciers observed retre
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of 0.1° and 5 days (Kaiser et al.
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Fig. 3.1. (a) Yearly mean SSTAs in
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(Fig. 3.3c). It is interesting that
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strong there, consistent with anoma
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cont'RECENT ADVANCES IN OUR UNDERST
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is to cause SST to rise if oceanic
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egions around the subtropical salin
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Fig 3.17. Principal empirical ortho
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Fig. 3.19. Daily estimates of the s
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Fig. 3.22. (top) The 2009 SSH anoma
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to update the CO 2climatology, ther
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µmol kg -1 or about half of the ac
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Fig. 3.31. (a) Average MODIS-Aqua C
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latitudes, chlorophyll and thermal
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Fig. 4.4. (a) Anomalous 850-hPa win
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(Fig. 4.6). These include four MJO
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Fig. 4.8. NOAA’s ACE index expres
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Fig. 4.14. ASO 2009: Anomalous 200-
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Fig. 4.17. The tracks of all TCs th
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Several previous studies have shown
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followed by TY Linfa and TS Nangka
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The Philippines were severely affec
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The historical SIO TC data is proba
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Fig. 4.26. Global anomalies of TCHP
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degree resolution NASA TRMM rainfal
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F i g. 4.32 . TRMM (a) mean and (b)
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THE forgotten sub-BASIN—THE centr
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5. THE ARCTIC—J. Richter-Menge, E
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and North America (south of 55° la
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Ramaswamy, V., M. D. Schwarzkopf, W
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——, ——, T. C. Peterson, and
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Wang, L., C. Derksen, and R. Brown,
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Monthly average temperature anomali