Tanzania. General Climate. UNDP Climate Change Country Profiles. C. McSweeney 1, M. New 1,2 and G. Lizcano 1
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1 UNDPClimateChangeCountryProfiles Tanzania C.McSweeney 1,M.New 1,2 andg.lizcano 1 1.SchoolofGeographyandEnvironment,UniversityofOxford. 2.TyndallCentreforClimateChangeResearch GeneralClimate Tanzanialiesjustsouthoftheequator,at111 Sandhasatropicalclimatewithregionalvariations duetotopography.withtheexceptionofanarrowcoastalstrip,mostoftanzaniaishighland.the greaterpartoftanzaniaisacentralplateauofaround m,punctuatedwithmountain ranges(includingkilimanjaro,5895m).thecoastalregionsoftanzaniaarewarmandhumid,with temperatures25to17 Cthroughmostoftheyear,dippingjustbelow25 Cinthecoolestmonths (JJAS).Thehighlandregionsaremoretemperate,withtemperaturesaround2023 Cthroughout theyear,droppingbyonlyadegreeorsoinjjas. SeasonalrainfallinTanzaniaisdrivenmainlybythemigrationoftheInterTropicalConvergence Zone(ITCZ),relativelynarrowbeltofverylowpressureandheavyprecipitationthatformsnearthe earth sequator.theexactpositionoftheitczchangesoverthecourseoftheyear,migrating southwardsthroughtanzaniainoctobertodecember,reachingthesouthofthecountryinjanuary andfebruary,andreturningnorthwardsinmarch,aprilandmay.thiscausesthenorthandeastof Tanzaniaexperiencestwodistinctwetperiods the short rainsinoctobertodecemberandthe long rainsinmarchtomay,whilstthesouthern,westernandcentralpartsofthecountry experienceonewetseasonthatcontinuesoctoberthroughtoaprilormay.theamountofrainfall fallingintheseseasonsisusually50200mmpermonthbutvariesgreatlybetweenregions,andcan beasmuchas300mmpermonthinthewettestregionsandseasons.themovementsoftheitcz aresensitivetovariationsinindianoceanseasurfacetemperaturesandvaryfromyeartoyear, hencetheonset,durationandintensityoftheserainfallsvaryconsiderablyinterannually.oneof themostwelldocumentedoceaninfluencesonrainfallinthisregionistheelniñosouthern Oscillation(ENSO).ElNiñoepisodesusuallycausegreaterthanaveragerainfallsintheshortrainfall season(ond),whilstcoldphases(laniña)bringadrierthanaverageseason. 1
2 RecentClimateTrends Temperature Meanannualtemperaturehasincreasedby1.0 Csince1960,anaveragerateof0.23 Cper decade.thisincreaseintemperaturehasbeenmostrapidinjfandslowestinjjas. Dailytemperatureobservationsshowonlysmallincreasingtrendsinthefrequencyhot days 1,butmuchlargerincreasingtrendsinthefrequencyofhotnights. o Theaveragenumberof hot daysintanzaniahasonlyincreasedsignificantlyindjf whentheaveragenumberofhotdjfdayshasincreasedby2.5dayspermonth(an additional8.2%ofdjfdays)between1960and2003. o Theaveragenumberof hot nightsperyearincreasedby50(anadditional13.6%of nights)between1960and2003.therateofincreaseisseenmoststronglyindjf whentheaveragenumberofhotdjfnightshasincreasedby6dayspermonth(an additional19.8%ofdjfnights)overthisperiod. Thefrequencyofcold 2 dayshasnotchangeddiscernibly,despitetheobservedincreasesin meantemperature.thefrequencyofcoldnightshas,however,decreasedsignificantlyinall seasons. o Theaveragenumberof cold nightsperyearhasdecreasedby34(9.3%ofdays). ThisrateofdecreaseismostrapidinDJFwhentheaveragenumberofcoldDJF nightshasdecreasedby3.6nightspermonth(11.5%ofdjfnights)overthisperiod. Precipitation ObservationsofrainfalloverTanzaniashowstatisticallysignificantdecreasingtrendsin annual,andjjasandmamrainfall.annualrainfallhasdecreasedatanaveragerateof 2.8mmpermonth(3.3%)perdecade.Thegreatestannualdecreaseshaveoccurredinthe southernmostpartsoftanzania.mamandjjasrainfallshavedecreasedby4.0and0.8mm permonthperdecade,respectively(3.0%and6.0%). Trendsintheextremeindicesbasedondailyrainfalldataaremixed.Thereisnostatistically significanttrendintheproportionofrainfalloccurringinheavy 3 events.1and5dayrainfall maximashowsmall,nonstatisticallysignificantdecreasingtrends.5dayeventsshowa significantincreasingtrendof+11.03mmperdecadeinmam. 1 Hot dayor hot nightisdefinedbythetemperatureexceededon10%ofdaysornightsincurrentclimateofthatregionandseason. 2 Cold daysor cold nightsaredefinedasthetemperaturebelowwhich10%ofdaysornightsarerecordedincurrentclimateofthat regionorseason. 3 A Heavy eventisdefinedasadailyrainfalltotalwhichexceedsthethresholdthatisexceededon5%ofrainydaysincurrentthe climateofthatregionandseason. 2
3 GCMProjectionsofFutureClimate Temperature Themeanannualtemperatureisprojectedtoincreaseby1.0to2.7 Cbythe2060s,and1.5 to4.5 Cbythe2090s.Therangeofprojectionsbythe2090sunderanyoneemissions scenariois C. Allprojectionsindicateincreasesinthefrequencyofdaysandnightsthatareconsidered hot incurrentclimate. o Annually,projectionsindicatethat hot dayswilloccuron1940%ofdaysbythe 2060s,and1965%ofdaysbythe2090s. o Nightsthatareconsidered hot fortheannualclimateof197099areprojectedto increasemorequicklythathotdays,occurringon3068%ofnightsbythe2060sand 3591%ofnightsbythe2090s.Nightsthatareconsideredhotforeachseasonby standardsareprojectedtoincreaseparticularlyrapidlyinDJF,occurringon 4799%ofnightsintheseasonbythe2090s. Allprojectionsindicatedecreasesinthefrequencyofdaysandnightsthatareconsidered cold incurrentclimate.theseeventsareexpectedtobecomeexceedinglyrare,withcold daysoccurringon04%ofdaysandcoldnightsoccurringonamaximumof1%ofdays,and notatallunderthetwohigheremissionsscenarios,bythe2090s. Precipitation Projectionsofmeanrainfallarebroadlyconsistentinindicatingincreasesinannualrainfall. Theensemblerangespanschangesof4to+30%bythe2090s,andensemblemedian changesof+7to+14%. Theannualincreasesinrainfallaresimilaracrossthewholecountry,buttheseasonal patternsofchangearemorecomplex.increasesinjfrainfallaffectmostofthecountrybut particularlytheverysouth,whilsttheincreasesinmamandsonrainfallaregreatestinthe northernregionsofthecountry.injjas,rainfallincreasesintheverynorthofthecountry, butdecreasesincentralandsoutherntanzania.thispatternsuggeststhatrainfallgenerally increasesinthewetseason(s)ofeachregion. Themodelsconsistentlyprojectoverallincreasesintheproportionofrainfallthatfallsin heavyevents.theincreasesrangefrom1to14%inannualrainfallbythe2090s.increases affectmostofthecountryintheseasonsjf,mamandson. Themodelsconsistentlyprojectincreasesin1and5dayrainfallmaximabythe2090sofup to24mmin1dayevents,and4to37mmin5dayevents.thelargestincreasesareseenin MAM. 3
4 OtherRegionalClimateChangeInformation Modelsimulationsshowwidedisagreementsinprojectedchangesintheamplitudeoffuture ElNiñoevents.Tanzania sseasonalrainfallcanbestronglyinfluencedbyenso,thus contributingtouncertaintyinclimateprojectionsforthisregion. ForfurtherinformationonclimateprojectionsforAfrica,seeChristensenetal.(2007)IPCC WorkingGroupIReport: ThePhysicalScienceBasis,Chapter11(RegionalClimate projections):section11.2(africa). 4
5 DataSummary Observed Mean Observed Trend Projectedchangesbythe 2030s Projectedchangesbythe 2060s Projectedchangesbythe 2090s Min Median Max Min Median Max Min Median Max Temperature (changein C ( C) perdecade) Changein C Changein C Changein C A Annual * A1B B A JF * A1B B A MAM * A1B B A JJAS * A1B B A OND * A1B B Precipitation (mmper month) (changein mmper decade) Changeinmmpermonth Changeinmmpermonth Changeinmmpermonth A Annual * A1B B A JF A1B B A MAM * A1B B A JJAS * A1B B A OND A1B B Precipitation(%) (mmper month) (changein% perdecade) %Change %Change %Change A Annual * A1B B A JF A1B B A MAM * A1B B A JJAS * A1B B A OND A1B B
6 Observed Mean Observed Trend Projectedchangesbythe 2030s Projectedchangesbythe 2060s Projectedchangesbythe 2090s Min Median Max Min Median Max Min Median Max % Frequency Changein frequency perdecade Future%frequency Future%frequency FrequencyofHotDays(TX90p) A2 **** **** **** Annual A1B **** **** **** B1 **** **** **** A2 **** **** **** JF 13.2 (1.91*) A1B **** **** **** (DJF) B1 **** **** **** A2 **** **** **** MAM A1B **** **** **** B1 **** **** **** A2 **** **** **** JJAS 11.1 (0.32) A1B **** **** **** (JJA) B1 **** **** **** A2 **** **** **** OND A1B **** **** **** B1 **** **** **** FrequencyofHotNights(TN90p) A2 **** **** **** Annual * A1B **** **** **** B1 **** **** **** A2 **** **** **** JF 13.2 (4.60*) A1B **** **** **** (DJF) B1 **** **** **** A2 **** **** **** MAM * A1B **** **** **** B1 **** **** **** A2 **** **** **** JJAS 9.4 (1.52) A1B **** **** **** (JJA) B1 **** **** **** A2 **** **** **** OND A1B **** **** **** B1 **** **** **** FrequencyofColdDays(TX10p) A2 **** **** **** Annual A1B **** **** **** B1 **** **** **** A2 **** **** **** JF 8.4 (0.47) A1B **** **** **** (DJF) B1 **** **** **** A2 **** **** **** MAM A1B **** **** **** B1 **** **** **** A2 **** **** **** JJAS 8.5 (0.15) A1B **** **** **** (JJA) B1 **** **** **** A2 **** **** **** OND A1B **** **** **** B1 **** **** **** FrequencyofColdNights(TN10p) A2 **** **** **** Annual * A1B **** **** **** B1 **** **** **** A2 **** **** **** JF 8.0 (2.68*) A1B **** **** **** (DJF) B1 **** **** **** A2 **** **** **** MAM * A1B **** **** **** B1 **** **** **** A2 **** **** **** JJAS 8.2 (2.35*) A1B **** **** **** (JJA) B1 **** **** **** A2 **** **** **** OND * A1B **** **** **** B1 **** **** ****
7 Observed Mean Observed Trend Projectedchangesbythe 2030s Projectedchangesbythe 2060s Projectedchangesbythe 2090s Min Median Max Min Median Max Min Median Max %totalrainfallfallinginheavyevents(r95pct) Changein% % perdecade Changein% Changein% A2 **** **** **** Annual A1B **** **** **** B1 **** **** **** A2 **** **** **** JF **** **** A1B **** **** **** (DJF) B1 **** **** **** A2 **** **** **** MAM **** **** A1B **** **** **** B1 **** **** **** A2 **** **** **** JJAS **** **** A1B **** **** **** (JJA) B1 **** **** **** A2 **** **** **** OND **** **** A1B **** **** **** B1 **** **** **** Maximum1dayrainfall(RX1day) Changein mm mmper Changeinmm Changeinmm decade A2 **** **** **** Annual **** **** A1B **** **** **** B1 **** **** **** A2 **** **** **** JF 29.8 (1.79) A1B **** **** **** (DJF) B1 **** **** **** A2 **** **** **** MAM **** **** A1B **** **** **** B1 **** **** **** A2 **** **** **** JJAS 8.6 (0.56) A1B **** **** **** (JJA) B1 **** **** **** A2 **** **** **** OND A1B **** **** **** B1 **** **** **** Maximum5dayRainfall(RX5day) Changein mm mmper Changeinmm Changeinmm decade A2 **** **** **** Annual A1B **** **** **** B1 **** **** **** A2 **** **** **** JF 52.2 (0.93) A1B **** **** **** (DJF) B1 **** **** **** A2 **** **** **** MAM * A1B **** **** **** B1 **** **** **** A2 **** **** **** JJAS 13.4 (1.39) A1B **** **** **** (JJA) B1 **** **** **** A2 **** **** **** OND A1B **** **** **** B1 **** **** **** *indicatestrendisstatisticallysignificantat95%confidence ****indicatesdataarenotavailable Bracketedtrendvaluesforextremesindicesindicatevaluesfortheclosestseasonsthatdataisavailable.Seedocumentation. 7
8 Figure 1: Trends in annual and seasonal mean temperature for the recent past and projected future. All values shown are anomalies, relative to the mean climate. Black curves show the mean of observed data from 1960 to 2006, Brown curves show the median (solid line) and range (shading) of model simulations of recent climate across an ensemble of 15 models. Coloured lines from 2006 onwards show the median (solid line) and range (shading) of the ensemble projections of climate under three emissions scenarios. Coloured bars on the right-hand side of the projections summarise the range of mean climates simulated by the 15 models for each emissions scenario. 8
9 Figure 2: Spatial patterns of projected change in mean annual and seasonal temperature for 10-year periods in the future under the SRES A2 scenario. All valuesare anomalies relative to the mean climate of In each grid box, the central value gives the ensemble median and the values in the upper and lower corners give the ensemble maximum and minimum. 9
10 Figure 3: Trends in monthly precipitation for the recent past and projected future. All values shown are anomalies, relative to the mean climate. See Figure 1 for details. 10
11 Figure 4: Spatial patterns of projected change in monthly precipitation for 10-year periods in the future under the SRES A2 scenario. All values are anomalies relative to the mean climate of See Figure 2 for details. 11
12 Figure 5: Trends in monthly precipitation for the recent past and projected future. All values shown are percentage anomalies, relative to the mean climate. See Figure 1 for details. 12
13 Figure 6: Spatial patterns of projected change in monthly precipitation for 10-year periods in the future under the SRES A2 scenario. All values are percentage anomalies relative to the mean climate of See Figure 2 for details. 13
14 Figure 7: Trends in Hot-day frequency for the recent past and projected future. See Figure 1 for details. 14
15 Figure 8: Spatial patterns of projected change in Hot-day frequency for 10-year periods in the future under the SRES A2 scenario. See Figure 2 for details. 15
16 Figure 9: Trends in hot-night frequency for the recent past and projected future. See Figure 1 for details. 16
17 Figure 10: Spatial patterns of projected change in hot-night frequency for 10-year periods in the future under the SRES A2 scenario. See Figure 2 for details. 17
18 Figure 11: Trends in cold-day frequency for the recent past and projected future. See Figure 1 for details. 18
19 Figure 12: Spatial patterns of projected change in cold-day frequency for 10-year periods in the future under the SRES A2 scenario. See Figure 2 for details. 19
20 Figure 13: Trends in cold-night frequency for the recent past and projected future. See Figure 1 for details. 20
21 Figure 14: Spatial patterns of projected change in cold-night frequency for 10-year periods in the future under the SRES A2 scenario. See Figure 2 for details. 21
22 Figure 15: Trends in the proportion of precipitation falling in heavy events for the recent past and projected future. All values shown are anomalies, relative to the mean climate. See Figure 1 for details. 22
23 Figure 16: Spatial patterns of projected change in the proportion of precipitation falling in heavy events for 10-year periods in the future under the SRES A2 scenario. All values are anomalies relative to the mean climate of See Figure 2 for details. 23
24 Figure 17: Trends in maximum 1-day rainfall for the recent past and projected future. All values shown are anomalies, relative to the mean climate. See Figure 1 for details. 24
25 Figure 18: Spatial patterns of maximum 1-day rainfall for 10-year periods in the future under the SRES A2 scenario. All values are anomalies relative to themean climate of See Figure 2 for details. 25
26 Figure 19: Trends in maximum 5-day rainfall for the recent past and projected future. All values shown are anomalies, relative to the mean climate. See Figure 1 for details. 26
27 Figure 20: Spatial patterns of projected change in maximum 5-day rainfall for 10-year periods in the future under the SRES A2 scenario. All values are anomalies relative to the mean climate of See Figure 2 for details. 27
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