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What makes up Geographical pattern For temperature
Latitude - major determinant of temp. Season important due to tilt of Earth
Distance from ocean- water has higher water storage capacity, buffers changes & continental locations gain or lose heat more quickly
Elevation- 100 meters up make up 1 degree of latitude. Tree line growing season temp across the globe is relatively consistent
Seasonality
Impact on temperature on growth factors
Day length
-Number of days when above ground growth is possible (estimated as number of days between the average date of the last killing frost in the spring and first killing frost in the fall)
Heat Sum Index
-Amount of heat that plants are exposed to
-Product of the number of days over a base temp and the number of daylight hours at that temp
-Imporatnt factor for flowering and bud burst in the spring (Variation across species)
Temperatures at the soil surface
What drives daytime vs nighttime temps
Important drivers of ecosystem productivity
What influences soil temperature
What drives daytime vs nighttime temps
Day time: Regulated by SOLAR RADIATION
Night time: Determine by the amount of HEAT ABSORBED BY TERRESTRIAL OBJECTS and the ability of those objects to hold heat
Important drivers of ecosystem productivity
Biological activity of roots and their associated microbial organism
Nutrient and water uptakes
Mineralization and Decomposition
What influences soil temperature
1.) Soil Water Content
2.) Soil Properties
-Thermal conductivity and Particle Size
3.) Leaf Litter
Microclimate and more
Variation in climatic parameters within a small spatial scale)
Factors include abiotic and biotic
Abiotic- Topography, elevation, soil props, water bodies, sun exposure
Biotic- Stand Structure, Forest type, Density (greater density, greater modulating effect), Forest Age (old growth forests have the greatest ability to moderate temp use to complex structures
Consider all this for management
Frost Pockets/ Valley Fog
Influence of Temp on Photosynthesis
All temps have a temp range where they preform best (photosynthesis will decrease outside this range)
Extreme cold and heat
Cold tolerance
What happens when plants experience extreme cold or heat
Cold:
Slows down cell processes
Causes plasma membrane to lose function
Ice damage
Heat:
Proteins lose function (help by helping denatured proteins to reform quickly)
Cells dry out
Cold tolerance
Unprotected cells vs protected cells
Protected:
Ice nucleating proteins
Antifreeze proteins
Solute transfer
Membrane protection
Plant dormancy
Process of making the plant more tolerant to cold temperatures
Triggered by short days
Pre Dormancy- Reversible (Startch starts to accumulate in roots)
True Dormancy- Production of proteins, membrane lipids, and compounds for frost tolerance
Many plants skip true dormancy they go from pre to post
Plasticity, Acclimation, and Cold tolerance in plants
Frost hardiness is costly for trees, many species of Eastern trees exhibit variation in hardiness based on where in their range they are
Ex: Rhododendrons (Leaf Rolling)
Breaking Dormancy
Most temperate woody species require a period of cold temps before growth can resume in the spring. Once the chilling requirement is met, spring growth processes are temp dependent.
Stratification
Chilling requirements in seeds. How they break dormancy
All About Winter Cold Hardiness
Important in determining the Northern Limits of a species:
Timing of a bud burst in relation to spring temperatures (Spring frost are more limiting than winter because the plant has broke dormancy)
Trade offs in flushing time