Compound droughts and hot events or extremes (CDHEs) may lead to larger repercussions
than do individual extremes. Due to the disastrous impacts and increased risk of these …

Hydroclimatic changes associated with global warming over the past 50 years have been
documented widely, but physical landscape responses are poorly understood thus far …

Abstract Between 2000 and 2014, annual Colorado River flows averaged 19% below the
1906–1999 average, the worst 15‐year drought on record. At least one‐sixth to one‐half …

As the climate changes, drought may reduce tree productivity and survival across many
forest ecosystems; however, the relative influence of specific climate parameters on forest …

The causes of the California drought during November–April winters of 2011/12–2013/14
are analyzed using observations and ensemble simulations with seven atmosphere models …

Global warming driven by rising greenhouse-gas concentrations is expected to cause wet
regions of the tropics and mid to high latitudes to get wetter and subtropical dry regions to …

In recent decades, intense droughts, insect outbreaks, and wildfires have led to decreasing
tree growth and increasing mortality in many temperate forests. We compared annual tree …

The typically sparse distribution of weather stations in mountainous terrain inadequately
resolves temperature variability. Accordingly, high‐resolution gridding of climate data (for …

Unlike the commonly used relative humidity, vapor pressure deficit (VPD) is an absolute
measure of the difference between the water vapor content of the air and its saturation value …

Across the Upper Missouri River Basin, the recent drought of 2000 to 2010, known as the
“turn-of-the-century drought,” was likely more severe than any in the instrumental record …