phenological mismatch
When organisms dependent on synchronized milestones adapt to environmental changes at different rates, causing their reproductive, feeding, and/or migration patterns to become asynchronous
climate change
Global temperature increase and associated changes in precipitation patterns and extreme weather affecting ecosystems worldwide
climate-induced range shifts
Changes in species geographic distributions in response to changing climate conditions, typically involving movement to higher elevations or latitudes
aridity
Environmental condition characterized by limited water availability
microclimate heterogeneity
Variation in microclimatic conditions across small spatial scales, including differences in slope, aspect, and elevation that create diverse microclimatic niches
seasonal cycle
meteorology
drought resilience
Ability of forest ecosystems to maintain function during water-limited conditions through adaptive water use strategies
atmospheric boundary layer
The lowest part of the atmosphere directly influenced by the Earth's surface
monsoon
phenological mismatch
Food availability timing related to snow melt and vegetation growth potentially mismatched with juvenile foraging periods
North American Monsoon
Seasonal precipitation system occurring July-September in the central Rocky Mountains bringing significant rainfall to Colorado River headwater basins
extreme climatic events
Meteorological events that are rare for a particular place or time of year and can have major ecological impacts
frost exposure
orographic turbulence
Atmospheric turbulence generated by airflow over mountainous terrain leading to enhanced mixing and modified precipitation processes
blowing snow
climate change effects on behavior
How changing weather patterns and climate conditions influence animal behavioral strategies
permafrost
thermally driven upvalley wind
Valley wind that develops due to differential heating between valley floor and surrounding slopes, typically flowing upslope during daytime
Last Glacial Maximum
The most recent time during the last glacial period when ice sheets were at their greatest extent
bio-organic INPs
El Niño-Southern Oscillation
Climate pattern characterized by variations in sea surface temperatures in the Pacific Ocean that affects global weather patterns
gustnadoes
last interglacial period
The most recent period in Earth's history (~116-130 ka) when temperatures were persistently warmer than today, specifically the Eemian period at 125 ka
surface inversion
Heinrich Event 1
biological INPs
boreal greening
Projected increase in high-latitude forest growth due to warming temperatures
complex terrain
Mountainous regions with significant topographic variability that influences weather and climate processes
earlier starts to the summer season
orbital parameters
precipitation variability
Variation in rainfall patterns between years affecting plant growth and flower production
500mb pressure systems
Late Wisconsin
Millennium drought
The ongoing drought period in the Upper Colorado River Basin from 2000 to present, characterized by reduced precipitation and increased temperatures
Pinedale glaciation
The most recent major glaciation in the Rocky Mountains during the late Pleistocene
Pinedale maxima
UV radiation exposure
Exposure to ultraviolet radiation that increases with elevation and can damage plant tissues
aerosol layer
Atmospheric layer with elevated concentration of aerosol particles, detectable through lidar backscatter measurements
atmospheric soot emissions
Ten percent of all annual atmospheric soot emissions in Northern Hemisphere are from boreal wildfires
climate change
Anthropogenic environmental change expected to alter soil moisture availability and increase nitrogen deposition
climate change
Global warming and extreme weather events that threaten marmot survival through increasing temperature and changing precipitation patterns
climate change impacts on hibernation timing
Earlier emergence from hibernation in mid-April, more than a month earlier than in the 1970s, due to climate change effects
convective boundary layer
Turbulent atmospheric layer near surface that develops during daytime heating, characterized by well-mixed conditions and active convection
dendritic growth layer (DGL)
dust-on-snow
early reversal
fall streaks
fine-scale weather variation
Short-term (2-4 week) variation in temperature and precipitation that may interact with long-term climate change effects
foresummer drought
Early season dry period that occurs after snowmelt and lasts until the start of the summer monsoon season
