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upstream portion of a river basin can also extend For example, the supply of some economic good ldo ownstream as reduced streamflow may result in (e.g., water, hay, hydroelectric power) is weather n lo o c we tateirorxness , erevvoeinratnhdouggrhoum ndwater levels at downstream dependent. In most instances, the dema ist in this portion oef te tohreolboagsiicna . lRde ro duug ct h io tndsoe in sagn oo d d /o irsipnecrrecaasp in it gaacsoansru es mup lt tioofni . n T cr heearse in fo grnpd for tha e, opdu ro la utg io hnt reservoir and groundwater levels in downstream could be defined as occurring when the demand for tppuob rt liiocns of th duction, wraetcerre basin e at siuopnp , l ie msa , y h re ysdurlote in s transportati loenc , terr ic io us p o im w pacts on that good exceeds supply as a result of a weather-ot agricultu erre , parnod rceelpatteodfsdurpopu ly ghstho su rt p fa plol rt ( sSatnhde fo srtd ro n1g97s9y ) m . b T io hsiissctohn at m str heearms ectors. Conflicts between upstream and down exists between drought and human activities. Thus, 19 a9n4yfr wa o iv retrerb use an eaxsa in rss may mpl ienftrhree su U lt, as has been the case in the incidence of drought could increase be om th nei te MdisS so ta utreisR ( isveeerBOapsp in e ) r . cchha an ng gee in in so th ci e e ta flrevquu ln en er cayb il o it fytthoewpah te yrsischaolcaeuvseenot, faaw In h te errneartiivoen rs altrw an astceernddisnpau ti te osnaolfb te onrdaerriss , e su in chsiatsu atio rtages, or Middle East or between the United States ina th nesb ov o e th rg . r For example, nd increas aezs in o g il cea ro nsd io e n cr epao se oran la im nd a -l ucsaer ry pr in ac g tice , which exacerbates th ceaipsacsiu ty chanads Me T xi hceo . discussion up to this point has focused on the a es npdecviu al llnyerraeblielv it aynttoin fu t s ure droughts. This e m xa p m ac ptlseo is fodn is ste inctions between the types of drought during its Africa, Australia) and e in miaarre id a s re ogfiohnis ll y ( e o .g r ., sl Soopu in th g phase t or development pha drough otfd ty rpoeusgm ht a , y th deififnetre . rsree . l a During the termination terrain (e.g., Lesotho). understanding the termin Faitg io u ti roe nships between these During drought onset, agricul n tu p1h . a4se is sao ls fodurso ef uuglhitn .
DOI link for upstream portion of a river basin can also extend For example, the supply of some economic good ldo ownstream as reduced streamflow may result in (e.g., water, hay, hydroelectric power) is weather n lo o c we tateirorxness , erevvoeinratnhdouggrhoum ndwater levels at downstream dependent. In most instances, the dema ist in this portion oef te tohreolboagsiicna . lRde ro duug ct h io tndsoe in sagn oo d d /o irsipnecrrecaasp in it gaacsoansru es mup lt tioofni . n T cr heearse in fo grnpd for tha e, opdu ro la utg io hnt reservoir and groundwater levels in downstream could be defined as occurring when the demand for tppuob rt liiocns of th duction, wraetcerre basin e at siuopnp , l ie msa , y h re ysdurlote in s transportati loenc , terr ic io us p o im w pacts on that good exceeds supply as a result of a weather-ot agricultu erre , parnod rceelpatteodfsdurpopu ly ghstho su rt p fa plol rt ( sSatnhde fo srtd ro n1g97s9y ) m . b T io hsiissctohn at m str heearms ectors. Conflicts between upstream and down exists between drought and human activities. Thus, 19 a9n4yfr wa o iv retrerb use an eaxsa in rss may mpl ienftrhree su U lt, as has been the case in the incidence of drought could increase be om th nei te MdisS so ta utreisR ( isveeerBOapsp in e ) r . cchha an ng gee in in so th ci e e ta flrevquu ln en er cayb il o it fytthoewpah te yrsischaolcaeuvseenot, faaw In h te errneartiivoen rs altrw an astceernddisnpau ti te osnaolfb te onrdaerriss , e su in chsiatsu atio rtages, or Middle East or between the United States ina th nesb ov o e th rg . r For example, nd increas aezs in o g il cea ro nsd io e n cr epao se oran la im nd a -l ucsaer ry pr in ac g tice , which exacerbates th ceaipsacsiu ty chanads Me T xi hceo . discussion up to this point has focused on the a es npdecviu al llnyerraeblielv it aynttoin fu t s ure droughts. This e m xa p m ac ptlseo is fodn is ste inctions between the types of drought during its Africa, Australia) and e in miaarre id a s re ogfiohnis ll y ( e o .g r ., sl Soopu in th g phase t or development pha drough otfd ty rpoeusgm ht a , y th deififnetre . rsree . l a During the termination terrain (e.g., Lesotho). understanding the termin Faitg io u ti roe nships between these During drought onset, agricul n tu p1h . a4se is sao ls fodurso ef uuglhitn .
upstream portion of a river basin can also extend For example, the supply of some economic good ldo ownstream as reduced streamflow may result in (e.g., water, hay, hydroelectric power) is weather n lo o c we tateirorxness , erevvoeinratnhdouggrhoum ndwater levels at downstream dependent. In most instances, the dema ist in this portion oef te tohreolboagsiicna . lRde ro duug ct h io tndsoe in sagn oo d d /o irsipnecrrecaasp in it gaacsoansru es mup lt tioofni . n T cr heearse in fo grnpd for tha e, opdu ro la utg io hnt reservoir and groundwater levels in downstream could be defined as occurring when the demand for tppuob rt liiocns of th duction, wraetcerre basin e at siuopnp , l ie msa , y h re ysdurlote in s transportati loenc , terr ic io us p o im w pacts on that good exceeds supply as a result of a weather-ot agricultu erre , parnod rceelpatteodfsdurpopu ly ghstho su rt p fa plol rt ( sSatnhde fo srtd ro n1g97s9y ) m . b T io hsiissctohn at m str heearms ectors. Conflicts between upstream and down exists between drought and human activities. Thus, 19 a9n4yfr wa o iv retrerb use an eaxsa in rss may mpl ienftrhree su U lt, as has been the case in the incidence of drought could increase be om th nei te MdisS so ta utreisR ( isveeerBOapsp in e ) r . cchha an ng gee in in so th ci e e ta flrevquu ln en er cayb il o it fytthoewpah te yrsischaolcaeuvseenot, faaw In h te errneartiivoen rs altrw an astceernddisnpau ti te osnaolfb te onrdaerriss , e su in chsiatsu atio rtages, or Middle East or between the United States ina th nesb ov o e th rg . r For example, nd increas aezs in o g il cea ro nsd io e n cr epao se oran la im nd a -l ucsaer ry pr in ac g tice , which exacerbates th ceaipsacsiu ty chanads Me T xi hceo . discussion up to this point has focused on the a es npdecviu al llnyerraeblielv it aynttoin fu t s ure droughts. This e m xa p m ac ptlseo is fodn is ste inctions between the types of drought during its Africa, Australia) and e in miaarre id a s re ogfiohnis ll y ( e o .g r ., sl Soopu in th g phase t or development pha drough otfd ty rpoeusgm ht a , y th deififnetre . rsree . l a During the termination terrain (e.g., Lesotho). understanding the termin Faitg io u ti roe nships between these During drought onset, agricul n tu p1h . a4se is sao ls fodurso ef uuglhitn .
ABSTRACT