Growing pressure on sustainable water resource allocation in the context of global
development and rapid environmental change demands rigorous knowledge of how …

Palaeoenvironmental reconstructions with temporal coverages extending beyond Marine
Isotope Stage (MIS) three are scarce within the data sparse region of Chukotka, Far East …

The ongoing 22‐year drought in the Upper Colorado River Basin (UCRB) has been
extremely severe, even in the context of the longest available tree‐ring reconstruction of …

Water level changes result from a variety of geological, biological or climatic processes.
Many of these changes occur over long periods of time; however, some may be rapid or …

The premise of this article is that climate effects on lakes can be quantified most effectively
by the integration of process‐oriented limnological studies with paleolimnological research …

Predicting vegetation shifts under climate change is a challenging endeavor, given the
complex interactions between biotic and abiotic variables that influence demographic rates …

Reconstructing climate from lake sediments can be challenging, because the response of
lakes and various components of lake systems are mediated by non-climatic factors, such as …

The availability of water shapes life in the western United States, and much of the water in
the region originates in the Rocky Mountains. Few studies, however, have explicitly …

Regime shifts in lake ecosystems can occur in response to both abrupt and continuous
climate change, and the imprints they leave in paleolimnological records allow us to …

Regime shifts are generally defined as the point of 'abrupt'change in the state of a system.
However, a seemingly abrupt transition can be the product of a system reorganization that …