The premise that the intensity of biotic interactions decreases with increasing latitudes and
elevations is broadly accepted; however, whether these geographical patterns can be …

The expansion of shrubs and trees across high‐latitude ecosystems is one of the most
dramatic ecological manifestations of climate change. Most of the work quantifying these …

The near‐surface air temperature lapse rate is the predominant source of spatial
temperature variability in mountains and controls snowfall and snowmelt regimes, glacier …

Air temperature changes as a function of elevation were analyzed in a valley of the Spanish
Pyrenees. We analyzed insolation, topography and meteorological conditions in order to …

It is challenging to develop observationally based spatial estimates of meteorology in Alaska
and the Yukon. Complex topography, frozen precipitation undercatch, and extremely sparse …

Contributory citizen science programs focused on ecological monitoring can produce fine-
grained and expansive data sets across spatial and temporal scales. With this data …

To know the vertical distribution of air temperature is complex, and this is necessary for
different applications. The main explanatory variable of air temperature is elevation above …

High-latitude systems in northwestern Canada and Alaska have warmed rapidly. The aim of
this study was to examine how a remotely sensed proxy of vegetation productivity varied …

The spatiotemporal variations in spring onset were evaluated based on a satellite-derived
enhanced vegetation index (EVI), land surface temperature, and snow cover from 2000 to …

As an important indicator of climate change, precipitation variability is critical to the
ecological environment in arid and semi-arid mountains. This study examined the variability …