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A lo t w la n rainfall, covering all of the southern tropical tdheantcetsic. Furthermore, there are observational evi than c th au tsheatdrtohueg spatial scale of the rainfall anomalies extends e Nordeste h ts over the Nordeste is much larger 5° N, exftreonm di ntghewittrso el pfi . estw c Th a a rd leAaotvlnaonmt al er tihcobuestw ra e infall pattern (No e centr eanlA 5° m S az aonnd but T b io hreean fr l nd Shukla 1996). the histo oam rg e s ta in te htoomso ta gteenien ity of the rainfall distri Figure 5.4g . raImtissro ea f di a ly nnnuoatl th rea in Nfo al rldedsi te st r is ibsuhto io wnnb in y R ex io tr eGmreanddreoudgoh Norte bears ic e th aeb le la rign Figure 5.4 that cent of the clima ttso lo (a g n ic naulaalnrnau in aflap ll r e le esssttfh re aqnue5n0cypo er fyCeeaarrsa , w P it ahr ai tboat , a l an adn nu Paelr nambuco ecx ip pietr ation), whil rainfall slightly i en acbeovmeoo re esalrioguhn tl dyb th el eowmena ormal than years with precipitation r comparison, the n h (F is itgougrream5 .4) o . f Fo arnntuhael sa ra kien fa o ll f
DOI link for A lo t w la n rainfall, covering all of the southern tropical tdheantcetsic. Furthermore, there are observational evi than c th au tsheatdrtohueg spatial scale of the rainfall anomalies extends e Nordeste h ts over the Nordeste is much larger 5° N, exftreonm di ntghewittrso el pfi . estw c Th a a rd leAaotvlnaonmt al er tihcobuestw ra e infall pattern (No e centr eanlA 5° m S az aonnd but T b io hreean fr l nd Shukla 1996). the histo oam rg e s ta in te htoomso ta gteenien ity of the rainfall distri Figure 5.4g . raImtissro ea f di a ly nnnuoatl th rea in Nfo al rldedsi te st r is ibsuhto io wnnb in y R ex io tr eGmreanddreoudgoh Norte bears ic e th aeb le la rign Figure 5.4 that cent of the clima ttso lo (a g n ic naulaalnrnau in aflap ll r e le esssttfh re aqnue5n0cypo er fyCeeaarrsa , w P it ahr ai tboat , a l an adn nu Paelr nambuco ecx ip pietr ation), whil rainfall slightly i en acbeovmeoo re esalrioguhn tl dyb th el eowmena ormal than years with precipitation r comparison, the n h (F is itgougrream5 .4) o . f Fo arnntuhael sa ra kien fa o ll f
A lo t w la n rainfall, covering all of the southern tropical tdheantcetsic. Furthermore, there are observational evi than c th au tsheatdrtohueg spatial scale of the rainfall anomalies extends e Nordeste h ts over the Nordeste is much larger 5° N, exftreonm di ntghewittrso el pfi . estw c Th a a rd leAaotvlnaonmt al er tihcobuestw ra e infall pattern (No e centr eanlA 5° m S az aonnd but T b io hreean fr l nd Shukla 1996). the histo oam rg e s ta in te htoomso ta gteenien ity of the rainfall distri Figure 5.4g . raImtissro ea f di a ly nnnuoatl th rea in Nfo al rldedsi te st r is ibsuhto io wnnb in y R ex io tr eGmreanddreoudgoh Norte bears ic e th aeb le la rign Figure 5.4 that cent of the clima ttso lo (a g n ic naulaalnrnau in aflap ll r e le esssttfh re aqnue5n0cypo er fyCeeaarrsa , w P it ahr ai tboat , a l an adn nu Paelr nambuco ecx ip pietr ation), whil rainfall slightly i en acbeovmeoo re esalrioguhn tl dyb th el eowmena ormal than years with precipitation r comparison, the n h (F is itgougrream5 .4) o . f Fo arnntuhael sa ra kien fa o ll f
ABSTRACT