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Currency [0]/Explanatory TextG5Explanatory Text % 0Good;Good  a%1 Heading 1G Heading 1 I}%O2 Heading 2G Heading 2 I}%?3 Heading 3G Heading 3 I}%234 Heading 49 Heading 4 I}% 5InputuInput ̙ ??v% 6 Linked CellK Linked Cell }% 7NeutralANeutral  e%"Normal 8Noteb Note   9OutputwOutput  ???%????????? ???:$Percent ;Title1Title I}% <TotalMTotal %OO= Warning Text? Warning Text %XTableStyleMedium2PivotStyleLight16`1Sheet1RSheet2.TSheet3,T F$8(32 years of data, source: www.antarcticconnection.com )Month PrecipitationMean Windspeed(degC)(mm)(mph)JanFebMarAprMayJunJulAugSepOctNovDec7(26 years of data, source: www.antarcticconnection.com)VMONTHLY AVERAGES FOR TWO ANTARCTIC WEATHER STATIONS AND A STATION IN THE EUROPEAN ALPSWhat do you notice about the differences between the South Pole, part of the coast of Antarctica (McMurdo), and the station from the Alps?+(Data from 1981 to 2010, source: MetoSwiss) Avg. Temp Avg. Temp.4Piz Corvatsch, Switzerland, at 3,305 metres altitudeIhttp://www.meteoswiss.admin.ch/web/en/climate/swiss_climate/tabellen.htmlHAmundsen-Scott ANTARCTICA, McMurdo ANTARCTICA, Piz Corvatsch SWITZERLANDKey point: the precipitation is in the form of snow, but the milimetre measure is 'water-equivalent' (the amount of water if the snow was melted) IAmundsen-Scott Station, Antarctica (South Pole), at 2,835 metres altitude+McMurdo Station, Antarctica, near sea levelJYou can find the locations of each station on Google Maps or Google Earth.yFind out the average temperature for the whole year and the total yearly (annual) precipitation for each weather station.` hrYou could then draw a climate graph for Piz Corvatsch plotting monthly precipitation (as bars) and average monthly@maximum and minimum temperatures as points (connected by lines).eExtension task: You could visit the MeteoSwiss website at the address above to get more climate data.** +@+,*.jccB g2ɀ /"ENR  dMbP?_*+%&?'?(?)?MRICOH Aficio MP 2352 PCL 6  4dXX10DRM/~︥r[xTr0 }2h XC8{AJƞb._ oK04=􄆉@PՋQ=f_FL]BGgAa0=e{bLB%O"zsYrRwkou_" x .$3-4u P#p^ڿ9{M[ !'!ģ9a0cf+g5/W8-m(g߁y>ji$Y='9@X]z(S"7b~>>ba%6DOG4wUaRm!qt5P5=UR-n2`5ZH'8q.ǶUyl 6 F8Q 6J3³yJ89)9&:Ɖ)ʼT9\6ҲN΃FJ<?R|]]4)˴U1rOx+\K;]h~ۄZFX:$I" dXX??&U}  }  }  }  /      > >> > > > > >> > >> ? ? ?  > > > > >>> > > >>>> >>>> > > > > > > > >>> >>>  : ?  &F@  CV@  (D@  Ja@  &J@  Lffffff@   Q@  L@@  @X@  Lffffff@  Z@  M@  @Z@ M@ @@Z@ M@Ё@ @T@ I@e@ @S@ B@`@  Q@ :? &L@ >> > >>>>>  >>> > > > >>>>>>  >>>> >>> > > > >>>  >>> >>> .@*@@F D >zZNNZNZNNNNNZ *nZ !"#$%&'()*,-.   9@,@ ! !1(@1@ " "4.@0@ # #64@0@ $ $66@0@ % %9.@0@ &&:(@0@ ''7$@0@ ((21@,@ ))"$@(@ **(@(@ ,@# -@! .@" ***********>@ ' '' 7ggD g2ɀ S  dMbP?_*+%&?'?(?)?"??&U>@7ggD g2ɀ @U  dMbP?_*+%&?'?(?)?"??&U>@7ggD Oh+'0HPd|  D.AndersonBryony CollinsMicrosoft Excel@ 댏@Sxp@I ՜.+,0 PXp x Eton College Sheet1Sheet2Sheet3  Worksheets  !"#$%&'()*,-./012456789:Root Entry F-WorkbookUSummaryInformation(+DocumentSummaryInformation83