In the future, Earth will be warmer, precipitation events will be more extreme, global mean sea level will rise, and many arid and semiarid regions will be drier. Human modifications of landscapes will also occur at an accelerated rate as developed areas increase in size and population density. We now...
This study tested multiple hydrologic mechanisms to explain snowpack dynamics in extreme
rain-on-snow floods, which occur widely in the temperate and polar regions. We examined 26, 10 day
large storm events over the period 1992–2012 in the H.J. Andrews Experimental Forest in western Oregon,
using statistical analyses (regression, ANOVA, and...
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-arid mountain basin,
Ann. Glaciol., 32, 195–195, doi:10.3189/172756401781819751.
Marks, D., A
In many partially glacierized watersheds glacier recession driven by a warming climate could lead to complex patterns of streamflow response over time, often marked with rapid increases followed by sharp declines, depending on initial glacier ice cover and rate of climate change. Capturing such “phases” of hydrologic response is critical...
The West Antarctic Ice Sheet Divide (WAIS Divide, WD) ice core is a newly drilled, high-accumulation
deep ice core that provides Antarctic climate records of
the past ~68 ka at unprecedented temporal resolution. The
upper 2850 m (back to 31.2 ka BP) have been dated using
annual-layer counting. Here we...
The Last Interglacial (LIG) represents an invaluable case study to investigate the response of components of the Earth system to global warming. However, the scarcity of absolute age constraints in most archives leads to extensive use of various stratigraphic alignments to different reference chronologies. This feature sets limitations to the...