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m (e o .g s . t , cPoin tt s o is ctke nt 19w7i5 th , rainfall in the east and north negative values of the SOI usually coincide Ropelewski and Halpe M rt c1B9r8 id 7eanadnd19N 89 ic ) h . o R ll asi nf 1a9 ll 8 3 in , w cr iodpesypiree ld asd ( d N ro ic uhgoh ll t s ( 1F9 ig 8u5r ) e . T 3. h1e ) , c w or hrieclha ti l o ea ndsbettowwl ith the west is less strongly related to phenomenon. the year-to-year differences in yield and the ann eoewntNeim ch poelrlastu ( r 1989a) identified a pattern of sea ual rainfall fluc etuvaa ti r o ia nts io innitnhe th ceen In tr dailan an Odcseoaunthreer la stuerd fa c to e S is OI is 0 n parts Osc a il m la p ti le .4 6 e ( v n id = en4c0e ; stih gn at if ic tahnet at E1lpN er incoe -n S t) o . u T th heerrnetooftthheecEolnN tin in eon -t S . oTuhtihsep rn a tt O er snc il ilsato io n n ly awnedakalpyp related (e.g., N o ic n affects Australian wildlife and vegetation be a somewhat independent factor af efaercst in to g N na itcihvoe ll Asu1h9o8 ll 6 s , 1N9i8 ch 9obl , lsL1 im 99 p 1 us ). aFnodrN in iscthaonlcles , 1m9a8n8y , Aus N tr oat lian rainfall. severe, stralian plants are remarkably tolerant of climate, tshue rp E ri lsiN ng in ly o , -S g o iv u e th n er i n ts Oesfc fe il cltast io onn ha Asuastm ra a li jaonro fr reqauveon id ex t an tens se cvee iv st erad te rgoiuegsha ts r . e W es eslel-nd ti eavl el boepceadusteo le orfan th ceeF im ig puarcet3o . n2cs ro re dr ho pwysiteilm ds e , sneartiievseovfew ge hteaattioyn ie , ladns, daw ve il rdalg if eed . Sou H th oew rn Oscillation o . ughts caused by the El Nino-across Australia, and the SOI. The year-to-year dif Australia n we crle im atthee se a nd r ela tth io e nsh EilpsNb in e o tw -S e o en u the th rn e f th er eenecfe fe sctisno th fet re tw nd osvaan riables are plotted, to remove Oscillation uncovered? How have we progressed to duction of new cultivars d . cThhaengreeslas ti uocnhshaisptihseci le natrro - rNoiunto in -S eoiu ss tuhienrgnoOfsccillilm at a io te n ? forecasts, based on the El
DOI link for m (e o .g s . t , cPoin tt s o is ctke nt 19w7i5 th , rainfall in the east and north negative values of the SOI usually coincide Ropelewski and Halpe M rt c1B9r8 id 7eanadnd19N 89 ic ) h . o R ll asi nf 1a9 ll 8 3 in , w cr iodpesypiree ld asd ( d N ro ic uhgoh ll t s ( 1F9 ig 8u5r ) e . T 3. h1e ) , c w or hrieclha ti l o ea ndsbettowwl ith the west is less strongly related to phenomenon. the year-to-year differences in yield and the ann eoewntNeim ch poelrlastu ( r 1989a) identified a pattern of sea ual rainfall fluc etuvaa ti r o ia nts io innitnhe th ceen In tr dailan an Odcseoaunthreer la stuerd fa c to e S is OI is 0 n parts Osc a il m la p ti le .4 6 e ( v n id = en4c0e ; stih gn at if ic tahnet at E1lpN er incoe -n S t) o . u T th heerrnetooftthheecEolnN tin in eon -t S . oTuhtihsep rn a tt O er snc il ilsato io n n ly awnedakalpyp related (e.g., N o ic n affects Australian wildlife and vegetation be a somewhat independent factor af efaercst in to g N na itcihvoe ll Asu1h9o8 ll 6 s , 1N9i8 ch 9obl , lsL1 im 99 p 1 us ). aFnodrN in iscthaonlcles , 1m9a8n8y , Aus N tr oat lian rainfall. severe, stralian plants are remarkably tolerant of climate, tshue rp E ri lsiN ng in ly o , -S g o iv u e th n er i n ts Oesfc fe il cltast io onn ha Asuastm ra a li jaonro fr reqauveon id ex t an tens se cvee iv st erad te rgoiuegsha ts r . e W es eslel-nd ti eavl el boepceadusteo le orfan th ceeF im ig puarcet3o . n2cs ro re dr ho pwysiteilm ds e , sneartiievseovfew ge hteaattioyn ie , ladns, daw ve il rdalg if eed . Sou H th oew rn Oscillation o . ughts caused by the El Nino-across Australia, and the SOI. The year-to-year dif Australia n we crle im atthee se a nd r ela tth io e nsh EilpsNb in e o tw -S e o en u the th rn e f th er eenecfe fe sctisno th fet re tw nd osvaan riables are plotted, to remove Oscillation uncovered? How have we progressed to duction of new cultivars d . cThhaengreeslas ti uocnhshaisptihseci le natrro - rNoiunto in -S eoiu ss tuhienrgnoOfsccillilm at a io te n ? forecasts, based on the El
m (e o .g s . t , cPoin tt s o is ctke nt 19w7i5 th , rainfall in the east and north negative values of the SOI usually coincide Ropelewski and Halpe M rt c1B9r8 id 7eanadnd19N 89 ic ) h . o R ll asi nf 1a9 ll 8 3 in , w cr iodpesypiree ld asd ( d N ro ic uhgoh ll t s ( 1F9 ig 8u5r ) e . T 3. h1e ) , c w or hrieclha ti l o ea ndsbettowwl ith the west is less strongly related to phenomenon. the year-to-year differences in yield and the ann eoewntNeim ch poelrlastu ( r 1989a) identified a pattern of sea ual rainfall fluc etuvaa ti r o ia nts io innitnhe th ceen In tr dailan an Odcseoaunthreer la stuerd fa c to e S is OI is 0 n parts Osc a il m la p ti le .4 6 e ( v n id = en4c0e ; stih gn at if ic tahnet at E1lpN er incoe -n S t) o . u T th heerrnetooftthheecEolnN tin in eon -t S . oTuhtihsep rn a tt O er snc il ilsato io n n ly awnedakalpyp related (e.g., N o ic n affects Australian wildlife and vegetation be a somewhat independent factor af efaercst in to g N na itcihvoe ll Asu1h9o8 ll 6 s , 1N9i8 ch 9obl , lsL1 im 99 p 1 us ). aFnodrN in iscthaonlcles , 1m9a8n8y , Aus N tr oat lian rainfall. severe, stralian plants are remarkably tolerant of climate, tshue rp E ri lsiN ng in ly o , -S g o iv u e th n er i n ts Oesfc fe il cltast io onn ha Asuastm ra a li jaonro fr reqauveon id ex t an tens se cvee iv st erad te rgoiuegsha ts r . e W es eslel-nd ti eavl el boepceadusteo le orfan th ceeF im ig puarcet3o . n2cs ro re dr ho pwysiteilm ds e , sneartiievseovfew ge hteaattioyn ie , ladns, daw ve il rdalg if eed . Sou H th oew rn Oscillation o . ughts caused by the El Nino-across Australia, and the SOI. The year-to-year dif Australia n we crle im atthee se a nd r ela tth io e nsh EilpsNb in e o tw -S e o en u the th rn e f th er eenecfe fe sctisno th fet re tw nd osvaan riables are plotted, to remove Oscillation uncovered? How have we progressed to duction of new cultivars d . cThhaengreeslas ti uocnhshaisptihseci le natrro - rNoiunto in -S eoiu ss tuhienrgnoOfsccillilm at a io te n ? forecasts, based on the El
ABSTRACT