atmospheric soot emissions
Ten percent of all annual atmospheric soot emissions in Northern Hemisphere are from boreal wildfires
avalanche runout distance
The horizontal distance an avalanche travels from the starting zone to where it stops
bio-physical criteria
boundary layer mixing
Vertical mixing of air in the atmospheric boundary layer that affects aerosol concentrations and vertical distribution
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 effects on disease vectors
Expanding range and increased development of disease vectors like mosquitos, black flies, and biting midges due to warming temperatures
climate change effects on sociality
The hypothesis that warming climate and earlier snowmelt will increase sociality in bees by lengthening growing seasons and allowing development of multiple broods.
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
climate isolines
Lines of equivalent climate conditions that shift upslope with climate change
climate space
A physiological niche accounting for radiation, air temperature, wind, and humidity in which an animal can survive
cloud life cycle
cloud top height retrieval
Determination of cloud top altitude using atmospheric absorption in the oxygen A-band to infer pressure level
cold air pooling
Nighttime accumulation of cold dense air in valleys and topographic depressions due to radiative cooling and gravity drainage
convective boundary layer
Turbulent atmospheric layer near surface that develops during daytime heating, characterized by well-mixed conditions and active convection
degree-years
dendritic growth layer (DGL)
design-magnitude avalanche
A statistically-defined avalanche size (typically 100-300 year return period) used for engineering and land-use planning
dormant season climate
Climate conditions outside the growing season when plants are not actively growing
downward momentum transport
Vertical transfer of momentum from upper atmospheric levels down to near-surface levels through turbulent mixing or gravity waves
drying ratio
Precipitation efficiency measure based on integrated vapor transport normalization to evaluate microphysical scheme performance
dust delivery
dust-on-snow
early reversal
elevational gradient effects
Environmental changes with elevation including increased solar heating, low nocturnal temperatures, sudden intense storms, large interannual variations in snowpack, shorter growing season, lower plant...
energy storage
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
forced channeling
Mechanism where upper-level flow is channeled by valley sidewalls when convective boundary layer grows above ridge height, causing valley wind direction to align with upper-level flow
forest fuel loads
Quantified biomass of combustible material including duff, litter, and downed woody debris classified by time to ignition
foresummer drought
Early season dry period that occurs after snowmelt and lasts until the start of the summer monsoon season
freezing behavior
hygroscopic growth
ice water content
Mass of ice particles per unit volume of air, typically expressed in kg m⁻³
immersion mode
inertial instability
leaf temperature regulation
Regulation essential for photosynthesis, respiration, and water retention that impacts plant energy balance
light extinction
liquid layer base (LLB)
longwave CRE
maximum differential reflectivity (sZDRmax)
microclimate buffering
Protection of local environmental conditions from broader regional climate trends by fine-scale topographic features
microphysical parameterization
Representation of cloud microphysical processes in atmospheric models that control precipitation initiation and rates of snowfall
mixing height
moraine exposure age
multi-layer cloud systems
normalized rime mass
Quantitative measure of how heavily rimed an ice particle is, with M = 0 meaning completely unrimed and M → 1 meaning spherical graupel
orbital forcing
Climate changes driven by variations in Earth's orbital parameters affecting incoming solar radiation distribution
oxygen A-band absorption
Atmospheric absorption of solar radiation by molecular oxygen around 760nm wavelength used for pressure level determination
paleoglacier reconstruction
Reconstruction of past glacier extents and ice thickness using geomorphic evidence and numerical modeling
