Reconstructing climates of the past relies on a variety of evidence from a large number of
sites to capture the varied features of climate and the spatial heterogeneity of climate …

The loss of Arctic sea-ice has been implicated with severe cold and snowy mid-latitude
winters. However, the mechanisms and a direct link remain elusive due to limited …

Abstract The North Pacific is a zone of cyclogenesis that modulates synoptic-scale
atmospheric circulation, yet there is a paucity of instrumental and paleoclimate data to fully …

The stable isotope composition of precipitation has been widely applied to trace moisture
sources. In the westerly dominated areas of central Asia, the isotopic composition of …

Water resources in the northwestern Himalayas are influenced by the circulation of two
dominant weather systems: westerlies and southwest monsoons. The effect of climate …

Arctic amplification is a consequence of surface albedo, cloud, and temperature feedbacks,
as well as poleward oceanic and atmospheric heat transport. However, the relative impact of …

Recycled moisture contributed by continental evaporation and transpiration plays an
important role in regulating the hydrological processes and atmospheric humidity budget in …

Arctic sea-ice loss is emblematic of an amplified Arctic water cycle and has critical feedback
implications for global climate. Stable isotopes (δ18O, δ2H, d-excess) are valuable tracers …

Lake sediment oxygen isotope records (calcium carbonate-δ 18 O) in the western North
American Cordillera developed during the past decade provide substantial evidence of …

Precipitation over the southern rim of the Indian Himalayan Region (IHR) mainly occurs due
to two dominant synoptic weather systems: Indian winter (IWM: December, January …