<?xml version="1.0" encoding="UTF-8"?><xml><records><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Qin, Yue</style></author><author><style face="normal" font="default" size="100%">Hong, C. P.</style></author><author><style face="normal" font="default" size="100%">Zhao, H. Y.</style></author><author><style face="normal" font="default" size="100%">Stefan Siebert</style></author><author><style face="normal" font="default" size="100%">John T. Abatzoglou</style></author><author><style face="normal" font="default" size="100%">Laurie S. Huning</style></author><author><style face="normal" font="default" size="100%">Lindsey L. Sloat</style></author><author><style face="normal" font="default" size="100%">Sohyun Park</style></author><author><style face="normal" font="default" size="100%">Shiyu Li</style></author><author><style face="normal" font="default" size="100%">Darla K. Munroe</style></author><author><style face="normal" font="default" size="100%">Zhu, Tong</style></author><author><style face="normal" font="default" size="100%">Davis Steven J</style></author><author><style face="normal" font="default" size="100%">Nathaniel D. Mueller</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Snowmelt Risk Telecouplings for Irrigated Agriculture.&amp;nbsp;Nature Climate Change</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2022</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.nature.com/articles/s41558-022-01509-z</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">12</style></volume><pages><style face="normal" font="default" size="100%">1007–1015</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">Climate change is altering the timing and magnitude of snowmelt, which may either directly, or indirectly via global trade, affect agriculture and livelihoods dependent on snowmelt. Here we integrate sub-annual irrigation and snowmelt dynamics and a model of international trade to assess the global redistribution of snowmelt dependencies and risks under climate change. We estimate that 16% of snowmelt used for irrigation is for agricultural products traded globally, of which over 70% is from five countries. Globally, we observe a prodigious snowmelt dependence and risk diffusion, with particularly evident importing of products at-risk in western Europe. In Germany and U.K, respective local fraction of surface-water-irrigated agriculture supply exposed to snowmelt risks could increase from negligible to 16% and 10% under a 2°C warming. Our results reveal the trade-exposure of agricultural supplies, highlighting regions and crops whose consumption may be vulnerable to changing snowmelt even if their domestic production is not.</style></abstract><issue><style face="normal" font="default" size="100%">11</style></issue><notes><style face="normal" font="default" size="100%">&lt;p&gt;&lt;span&gt;Media Coverage:&amp;nbsp;&lt;a href=&quot;https://mp.weixin.qq.com/s/WPmRHAFT0Lv3rRy4B9zHEg&quot;&gt;北大科研&lt;/a&gt;；&lt;a href=&quot;https://mp.weixin.qq.com/s/DtNV_xtFyiqEUoTQOErGSw&quot;&gt;环境人Environmentor&lt;/a&gt;；&lt;span&gt;&amp;nbsp;&lt;a href=&quot;https://mp.weixin.qq.com/s/sYSrwI5p0uiEzDlmOcDKaw&quot;&gt;地学新文献&lt;/a&gt;；&lt;a href=&quot;https://cese.pku.edu.cn/kycg/145064.htm&quot;&gt;北京大学环境科学与工程学院&lt;/a&gt;&lt;br&gt;&lt;/span&gt;&lt;span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/p&gt;</style></notes></record></records></xml>