The Aral Sea Basin
Martin HoelzleMartina BarandunTobias BolchJoel FiddesAbror GafurovVeruska MuccioneTomas SaksMaria ShahgedanovaM AdnanG NabiM PoomeeA AshrafE AizenV AizenJ MelackV AizenE AizenV AizenE AizenV KuzmichenokV AizenE AizenJ MelackV AizenE AizenJ MelackJ DozierH ApelZ AbdykerimovaM AgalhanovaA BaimaganbetovN GavrilenkoL GerlitzO KalashnikovaK Unger-ShayestehS VorogushynA GafurovM BarandunM HussE BerthierA KbE AzisovT BolchR UsulbajevM HoelzleM BarandunM HussL SoldD FarinottiE AzisovN SalzmannR UsulbalievA MerkushkinM HoelzleT BolchT BolchS MarchenkoT BolchJ PetersA YegorovB PradhanM BuchroithnerV BlagoveshchenskyT BolchJ SheaL ShiyinM AzamY GaoS GruberW ImmerzeelA KulkarniH LiA TahirG ZhangY ZhangF BrunE BerthierP WagnonA KbD TreichlerM CaoJ CarrivickF TweedY ChenW LiH DengG FangZ LiP ChevallierB PouyaudM MojaiskyM BolgovO OlssonM BauerJ FroebrichV CondeG NicoP MateusJ CatalaoA Kontu
2019en
ABI
Annotatsiya
The alpine cryosphere, including snow, glaciers and permafrost, is critical to water management in the Aral Sea Basin (ASB) and larger Central Asia (CA) under the changing climate, as it stores large amounts of water in its solid forms. Most cryospheric components in the Aral Sea Basin are close to melting point, and hence very vulnerable to a slight increase in air temperature with significant consequences to long-term water availability and to water resources variability and extremes.
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