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Ice2 teku

Daga Wikipedia, Insakulofidiya ta kyauta.
Ice2 teku
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Iri ma'aikata
Ratsewar kankara cikin sauri tare da Shelf Ice Filchner-Ronne .
ice2 sea

Ice2sea wani shiri ne na binciken kimiyya wanda Shirin Tsari na 7 na Tarayyar Turai ya bada tallafi don nazarin tasirin sauyin yanayi kan glaciation da narkar da ƙanƙara a matakin teku. Aikin ice2sea, na haɗin gwiwar cibiyoyin bincike na 24, wanda Farfesa David Vaughan ya jagoranta, da nufin rage rashin tabbas acikin tsinkayen matakan teku wanda ke da mahimmancin tattalin arziki da zamantakewa ga Turai, musamman ma yadda manyan yankunan Turai na bakin teku ke ƙasa ko. kasa da mita sama da matakin teku.

Rahoton kwamitin sulhu na huɗu kan sauyin yanayi na shekara ta 2007 (IPCC) ya nuna alamar ƙanƙara a matsayin mafi girman rashin tabbas da ya rage a hasashen tashin matakin teku. Fahimtar mahimmancin tasirin ƙanƙara ya kasance "iyakantacce ne don tantance yuwuwarsu ko samar da mafi kyawun ƙima na babban iyaka don hawan matakin teku".

Ingantattun sakamakon kimiyya daga ice2sea da aka ciyar acikin rahoton IPCC na biyar (2013) don samar da ingantattun hasashen hawan teku.

Wannan yunƙurin ya ɗauki nauyin binciken da masana kimiyya daga Cibiyar Nazarin Polar da Ruwa ta Alfred Wegener a Jamus, wanda aka buga acikin Nature acikin 2012, wanda yayi hasashen bacewar 450,000 square kilometres (170,000 sq mi). babban Shelf Filchner-Ronne Ice a gabashin Antarctica a ƙarshen ƙarni wanda zai iya ƙara har zuwa 4.4 millimetres (0.17 in) na hawan teku a kowace shekara saboda narkewar shi kadai.

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