A 2000 year-long proxy and observational reconstruction of Central Asian climate

Central Asia (CA) is one of the most arid places on Earth and climate change threatens to disrupt the natural hydrologic systems that store its limited annual wet-season precipitation in glaciers and release it during the dry season. Warm/Wet and Cold/Dry periods recorded over the last 2000 years us...

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Bibliographic Details
Main Authors: Birkel, S. (Author), Mayewski, P. (Author), Rodda, C. (Author)
Format: Article
Language:English
Published: Elsevier Ltd 2019
Subjects:
CA
Online Access:View Fulltext in Publisher
LEADER 02605nam a2200577Ia 4500
001 10.1016-j.quascirev.2019.07.029
008 220511s2019 CNT 000 0 und d
020 |a 02773791 (ISSN) 
245 1 0 |a A 2000 year-long proxy and observational reconstruction of Central Asian climate 
260 0 |b Elsevier Ltd  |c 2019 
856 |z View Fulltext in Publisher  |u https://doi.org/10.1016/j.quascirev.2019.07.029 
520 3 |a Central Asia (CA) is one of the most arid places on Earth and climate change threatens to disrupt the natural hydrologic systems that store its limited annual wet-season precipitation in glaciers and release it during the dry season. Warm/Wet and Cold/Dry periods recorded over the last 2000 years using multiple paleoclimate proxy records reflect a local hydrocycle dominated by the Westerlies and moisture recycling within the Aral Sea catchment. The best tool for assessing recent climate trends is modern reanalysis modeling, ground-truthed by weather station data. Using the best-fit reanalysis, we find warming and drying trends have dominated the region over the last 115 years. Continued warming and drying in glacierized eastern CA during the critical spring season when glaciers typically increase in mass increase the likelihood that human infrastructure will be needed to impound wet-season precipitation. © 2019 
650 0 4 |a Aral Sea 
650 0 4 |a CA 
650 0 4 |a Calcium 
650 0 4 |a catchment 
650 0 4 |a Catchments 
650 0 4 |a Central Asia 
650 0 4 |a climate change 
650 0 4 |a Climate change 
650 0 4 |a Climate dynamics 
650 0 4 |a Climate dynamics 
650 0 4 |a Climate reanalyzer 
650 0 4 |a Climate reanalyzer 
650 0 4 |a climate variation 
650 0 4 |a Data analysis 
650 0 4 |a Data reduction 
650 0 4 |a dry season 
650 0 4 |a Earth (planet) 
650 0 4 |a Global historical climatology network 
650 0 4 |a Global historical climatology network (GHCN) 
650 0 4 |a Human infrastructure 
650 0 4 |a Hydrologic systems 
650 0 4 |a paleoclimate 
650 0 4 |a Paleoclimate proxy 
650 0 4 |a precipitation (climatology) 
650 0 4 |a proxy climate record 
650 0 4 |a Quaternary 
650 0 4 |a Quaternary 
650 0 4 |a Quaternary 
650 0 4 |a reconstruction 
650 0 4 |a seasonal variation 
650 0 4 |a water resource 
650 0 4 |a Water resources 
650 0 4 |a Water resources 
650 0 4 |a Weather stations 
650 0 4 |a wet season 
700 1 |a Birkel, S.  |e author 
700 1 |a Mayewski, P.  |e author 
700 1 |a Rodda, C.  |e author 
773 |t Quaternary Science Reviews