Lecture 3 climate Flashcards
Ecophysiology
adaptation of organisms physiology to environment
Plant ecophysiology
Mechanisms - sensing and responding to env. changes
Integration of responses to variable conditions
- radiation
- temp
- water …
phenotypic plasticity [change within lifetime]
animal ecophysiology
endocrine system
metabolism
thermoregulation
abiotic env.
Radiation Temperature Air Water Soil Chemicals
Climate
earth spherical = latitudinal variation in solar radiation absorption
Teperature and precipitation = vary with latititude
proportion of land or ocean = affects temp
totation around axis = air and water movment = wind and ocean currents
tilt of earths axis and orbit = seasons
altitude = surface uneven
climate involves
radiation [solar]
temperature
humidity
precipitation
Albedo effect
fraction of solar radiation reflected from earth back into space
measure of the reflectivity of earths surface (ice and snow reflect. forests and water absorb0
northen hemisphere greater proportion of land vs southern
northern warmer.
land radiates more heat to air above it
oceans absorb it more
circulation and precipitation
solar radiation determines atmospheric air circulation and percipitation patterns
air warmed. expands. becomes less dense. rises. cools. releases moisture (precipitation)
rising warm air replaced by surface air flowing in setting up atmospheric circulation cells
Coriolis effect
earths rotation = wind and ocean currents
prevailing wind meeting continents = large circular ocean currents called gyres
ocean currents transport heat
primary production and climate
primary production varies with latitude
primary production influences community diversity
Solar radiation
4 points
- Solar radiation drives global climate patterns
- 70% absorbed by atmosphere and earths surface
- Much of energy radiated from earths surface in form of heat
- Greenhouse gases e.g. CO2 trap most of radiated heat in atmosphere
Solar radiation
Albedo effect
5 points
- Albedo is fraction of solar radiation reflected from earth back into space
- Measure of reflectivity of earths surface
- Ice and snow reflect
- Water and forests absorb
- (high albedo = high reflection)
Solar radiation
Coriolis effect
5 points
- Earth rotation generates global wind and ocean currents
- Rotation fastest at equator
- Prevailing wind patterns drive ocean circulation patterns or currents
- Prevailing winds meeting continents set up large circular ocean currents called gyres
- Ocean currents affect earths climates by transporting heat
Solar radiation
Determines atmospheric air circulation and precipitation patterns
2 points
- Air warmed, expands, becomes less dense, rises, cools, releases moisture (precipitation)
- Rising warm air replaced by surface air flowing in, setting up atmospheric circulation cells
Temperature
Northern hemisphere slightly warmer and more variable in temperature than southern hemisphere
2 points
- North (greater proportion of land) - land radiates more heat to air above it
- South - Oceans absorb more heat