Ngelixa a ndice UV ye-8 imele umngcipheko omkhulu kwezempilo, iqela labaphandi abafunda ngemodeli yokusingqongileyo yaseMartian yeplanethi yethu ilinganise inqanaba lokurekhoda kwi IAndes. NgoDisemba 2003, isalathiso sagqitha kuma-43.
Umoya we Marte Imanzi kwaye ayinalo umaleko weozone ukukhusela naluphi na uhlobo lobomi kwimitha yelanga ephuma elangeni. Nangona kunjalo, kukho iindawo ze Umhlaba efana nomphezulu wentaba-mlilo kwiPlanethi ebomvu. Njengobungqina kwanele ukuthelekisa imifanekiso ethathwe Inqwenela kunye nezo mimandla zentlango yeAtacama.
Iibhiliyoni zeminyaka eyadlulayo xa Marte Kwakufudumele kwaye kunqabile kancinci kunanamhlanje, kunye nomoya ohambelana ngakumbi, iimeko kumphezulu kwakufuneka zisondele ngakumbi kwezo zifunyanwa namhlanje kwingingqi yaseLos Angeles. mlilo UAndean kwaye amachibi anetyuwa angumda wawo.
Ngale nto engqondweni, iqela le Abaphandi beNASA yahamba ngo-2003 yaya kwintaba-mlilo iLicancabur ebekwe kufutshane neikhweyitha kunye nomda phakathi kweBolivia neChile. Ngokuphakama phantse ngama-6000 m, le volcano inechibi le-crater apho kukho khona izinto eziphilayo Ukugqithisa.
Kwisiseko sayo, unokuncoma ii-expanses ezimbini ezinetyuwa, iLaguna Blanca kunye neLaguna Verde. Inkqubo ye- Iingcali zenzululwazi basandula ukupapasha inqaku kwiFrontiers kwiphephancwadi lezeNzululwazi ngezeNdalo bexela ukufunyanwa okumangalisayo kweso sihlandlo.
Ngenxa yokuphakama okuphezulu kunye umphezulu we-ozone ngokwendalo ebhityile kulo mmandla, abaphandi banethemba lokulinganisa ubungakanani obuphezulu bemitha ye-UV. Kodwa hayi ukuza kuthi ga ngoku ... Nge-29 kaDisemba ngo-2003, i Isalathiso se-UV ifikelele kwixabiso lama-43,3, oko kukuthi, isalathiso esiphakamileyo esakhe salinganiswa kumphezulu woMhlaba.
Ukuchaza le rekhodi, baphandi Bacebise ukudityaniswa kwezinto ezininzi. Akukho mngxunya we-ozone ngaphaya kweAndes, njengakwi-Antarctic, kodwa iiarosols kunye nemililo kulo mmandla Ilayisenisi banokuba negalelo ekunciphiseni ubume beozone ngelo xesha. Okokugqibela, yomelele Ingxaki yelanga yenzekile kwiiveki ezimbini phambi komlinganiselo. Oku kunokuba negalelo ekunciphiseni amanqanaba e-ozone kwaye, ukongeza, ezinye iincopho ze izinto ezikhutshwayo UV ziyenzeka emva kwesehlo esinjalo.