in Turkey and also in Macedonia, which recordedmonthly mean anomalies of greater than +4°C inplaces.(ii) PrecipitationThe year brought well-above-average precipitationover most of the southwestern Balkan Peninsula andsouthern Italy, exceeding 125% of normal in mostplaces (Fig. 7.30). In Croatia, rainfall was significantlybelow average in the East, while on the southernAdriatic coast precipitation was above the long-termmean. Some places in Turkey recorded 150% of theirannual average.Winter brought wetter-than-normal conditionsover most of Italy and the Balkan Peninsula, with theexception of Bulgaria (Fig. 7.33, DJF). January rainfallwas particularly high, with maxima in Greece andon the Adriatic coast of the Balkan Peninsula. LuqaAirport on Malta received its highest monthly rainfalltotal in 85 years (247 mm).The northern Balkan Peninsula experienced drierthan-normalconditions during spring, while wetterconditions occurred in the South. March precipitationin Athens was twice the normal. The eastern BalkanPeninsula had a very dry April, but places in northernItaly registered their second wettest April in 75 yearsor more, resulting in the flooding of the Po River.It was generally wet during June. Monthly averagetotals were exceeded by more than 25% with theexception of northern Italy, southern Greece andwestern Turkey, which were all very dry. July andAugust were mostly dry.Abundant rainfall occurred in southern Italyand Sardinia in September and October, whereasdrier-than-average conditions occurred in Tuscanyand northeastern Italy. Autumn was also very wet inthe southern and eastern parts of the Balkan Peninsula(Fig. 7.33, SON). September brought exceptionalrainfall totals to Athens (48 mm or 480% of 1961–90average). Serbia and northern parts of Bulgaria werevery wet during October.December was also generally wetter than averageacross the region. Several stations in northern Italyrecorded their wettest or second wettest December innearly 90 years, mainly due to an intense precipitationevent around Christmas. An exceptional local24-hr precipitation record was set in Makrinitsa incentral Greece, where 417.2 mm fell on 10 December.This corresponds to nearly half of the total rainfallfor <strong>2009</strong> at this station. Other locations also receivedexceptional precipitation on that day, resulting insignificant flooding and widespread damage.(iii) Notable eventsAn outbreak of cold air from Eastern Europebrought abundant snowfall over northern Italy from3–10 January. Temperatures dropped below 0°C inmany places. On 7 January, a snow depth of 26 cmwas reported in Milan.On 24 February, exceptionally heavy rainfall inMalta led to the cancellation of the National Carnivalgrand finale. A heavy storm over the western Mediterraneanwith gusts up to hurricane force, heavy rain,snowfall, and high seas followed on 4–6 March dueto a cut-off cyclone.From 20–22 June, an Atlantic disturbance affectedmost of Italy with heavy rainfall and strong winds.Daily precipitation on 21 June set new records at fourlocations which had 58 years of record.On 7–12 September, torrential rains and floodingaffected northwestern Turkey, with the heaviestrainfall in 80 years. Istanbul received 67 mm of rainwithin one hour on 9 September.A violent storm crossed southern Italy on 15–17September, flooding the city of Palermo (Sicily). On2 October, a storm dropped 70 mm of rain within sixhours in Messina, Sicily. Civil protection measurementstations recorded up to 300 mm of precipitationat mountainous sites, resulting in Italy’s worstmudslides in more than a decade.Abundant snowfalls occurred from 18–20 Decemberover northern parts of Italy, with depths up to 30cm. Subsequent warming and continuous rainfallresulted in rapid snowmelt causing extensive floodingin Tuscany just before Christmas.6) Eastern Europe—A. Obregón, P. Bissolli, J. J. Kennedy,and D. E. ParkerCountries considered in this chapter include:European Russia, Belarus, Ukraine, Moldova, andRomania.(i) TemperatureAnnual temperature anomalies over Eastern Europeranged between +1°C and +2°C (Fig. 29), withonly northern parts of European Russia recordinganomalies below +1°C. Parts of Romania exceededanomalies of +2°C. Moldova experienced its secondwarmest year in history, beaten only by 2007.Unlike most of Western Europe, Eastern Europeancountries experienced well-above-average temperaturesduring winter 2008/09 with anomalies surpassing+2°C (Fig. 7.32a).Spring temperature anomalies exceeded +1°C inwestern parts of Belarus, Ukraine, and Romania (Fig.S168 | juNE 2010
7.32b). April was particularly mild, although therewas a 10 to 20 day frost period in the Ukraine, notablyin eastern parts of the country. April was colder thannormal in European Russia (Fig. 7.34).Temperature anomalies reached +3°C in theUkraine during June and July, with a highest dailymaximum temperature for the region of 40°C. Summertemperature anomalies exceeded +1°C in Romaniaand Moldova, while anomalies in EuropeanRussia (+0.5°C) and Belarus were closer to normal.Autumn was characterized by the extremely mildmonths of September and November throughoutEastern Europe, with temperatures generally abovethe 90th percentile of the 1961–90 distribution. Thesemonths contributed to a seasonal anomaly of over+1°C in Romania, Moldova, Belarus, western partsof Ukraine, and northern parts of European Russia,while the eastern Ukraine and southern EuropeanRussia had anomalies in excess of +2°C (Fig. 7.32d).December temperatures in Belarus differed greatlyduring the month. The beginning of the month wasanomalously warm, with temperatures ranging from5°C–10°C above average. On 2 December, several locationsset new records for this day including Minsk,where temperatures reached 9.3°C, and Moscow(8.1°C), while in Moldova, it was the warmest nightfor a 2 December in the past 65 years. However thewarmest day in Moscow in December <strong>2009</strong> was on the6th, with 9.4°C. Remarkably, this value was measuredin the early morning and was a local record high forDecember. In sharp contrast, temperatures plungedbelow -15°C in the middle of December in many partsof Belarus, with temperatures falling as low as -27°C.The city of Perm in European Russia (in the lowlandsnear the Ural Mountains) experienced temperaturesas low as -41.4°C on 16 December, which was a newlocal record.(ii) PrecipitationPrecipitation totals in <strong>2009</strong> were generally closeto or above average for most of Eastern Europe (Fig.7.30). Only a few places in the Ukraine and centralEuropean Russia reported a rainfall deficit, recording60%–80% of average. Annual precipitation inthe north of European Russia exceeded 125% locally.Winter 2008/09 brought near-normal precipitation(Fig. 7.33, DJF) to the region; only a few scatteredlocations in Eastern Europe received considerablyabove-average seasonal totals. It was dry, however,in eastern parts of European Russia, with some areasreceiving less than 40% of their normal precipitation.Spring was dry in Moldova, with areas receivingonly 50%–75% of their average rainfall for the season.Similarly, parts of Romania and Ukraine were alsodry. April was particularly dry in the western regions.In Moldova, only 11.5 mm (26% of normal) of rainfallwas recorded, making April the second driest in 60years, second only to April 1974 (9mm). April was alsodrier than average in the Ukraine and Russia, wheremany stations reported monthly rainfall amountsbelow the 10th percentile.Summer was unusually wet in Belarus (secondwettest since 1936), mainly due to well-above-averageprecipitation during June and July. Minsk reporteda new record of monthly precipitation in June (187mm, more than twice normal). However, August hadonly about half of the normal precipitation totals inBelarus.Autumn precipitation was well above average overnorthern European Russia and Belarus, as well as inwestern parts of Romania and Ukraine (Fig. 7.33,SON), with October being particularly wet. Belarusreceived more than twice its normal rainfall and inRomania precipitation exceeded 150% of normal inmost places, with some areas exceeding 200%. Incontrast, autumn was dry in Moldova and in centralparts of Ukraine.There was a heavy snowfall in Moscow at the endof December, when 19 cm fell within 24 hours. A newrecord daily snowfall of 31 cm was set in Kyiv, beatingthe previous record by 3 cm. Ukraine saw heavy snowstorms in the first half of December.7) Middle East—A. Obregón, P. Bissolli, J. J. Kennedy, andD. E. ParkerCountries considered in this section include: Israel,Cyprus, Jordan, Lebanon, Syria, western Kazakhstan,Armenia, Georgia, and Azerbaijan.(i) TemperatureWarmer-than-average conditions prevailedthroughout the region during <strong>2009</strong>. The largestanomalies were experienced in Israel, Cyprus, and thewestern parts of Syria and Kazakhstan, with valuesgenerally ranging between +1°C and +2°C (Fig. 7.29).The largest positive temperature anomalies inwinter 2008/09 were in the Caucasian countries(i.e., Armenia, Georgia, Azerbaijan) and Israel. On9 February, temperatures above 30°C were recordedin parts of Israel, while between 13–16 Februarytemperatures reached 20°C in southern Armenia.While spring and summer temperatures were wellabove average in Jordan, Syria, Israel, and Cyprus,<strong>STATE</strong> <strong>OF</strong> <strong>THE</strong> <strong>CLIMATE</strong> <strong>IN</strong> <strong>2009</strong> juNE 2010 |S169
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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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Fig. 5.8. 2007-09 Atlantic water la
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d. Sea ice cover—D. Perovich, R.
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e. Land1) Vegetation—D. A. Walker
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Monthly average temperature anomali