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Plant Ecology - Chapter 17 Climate & Physiognomy
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The Abiotic Components of Ecosystems 1) Outside energy source 2) Physical factors that determine weather, climate weather, climate 3) Chemicals essential for life
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Outside Energy Source Powersphotosynthesis Warms earth Powers water cycle
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Physical factors that determine weather, climate HeatWindPrecipitationTopography
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Heat Location Reflection Retention
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Heat
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Heat
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Heat
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Heat
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Heat Daily temperatures can also vary dramatically in some habitats Deserts - dry air, loses heat rapidly High altitudes - thinner “blanket” of atmosphere
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Heat Long-term changes in earth’s orbit, position Collectively produce Croll-Milankovic effects on climate Orbit shape change Affects range of seasonal variation
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Heat Degree of tilt Affects range of seasonal variation
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Heat Direction of the tilt - the “wobble” Changes which hemisphere is pointed toward sun when orbit is closest to sun Affects severity of seasonal shift
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Wind and Precipitation Uneven heating Ascending, descending air masses - Hadley cell
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Modifiers Rotation of the globe - Coriolis effect Hadley, Ferrel cells, jet streams
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Modifiers Ocean currents, gyres induced by surface air mass movements
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Modifiers Topography - mountains Rain shadows
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Modifiers Topography - lakes Lake effect precipitation
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Modifiers Annual precipitation
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Modifiers
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Seasonal Patterns
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Multi-year Patterns 3-7-year El Nino Southern Oscillation
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Multi-year Patterns Combined ocean currents and jet stream
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Multi-year Patterns Milder winters along US-Canada border Increased winter storms in California Floods in SE, snow in SW mountains Decreased hurricane activity in Atlantic El Nino
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Multi-year Patterns More, stronger tornadoes in Midwest More, stronger hurricanes Drought, forest fires in SW La Nina
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Plant Physiognomy North-south gradient in vegetation form due to temperature West-east changes in response to precipitation
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Plant Physiognomy Evergreen broadleaf Deciduous broadleaf Evergreen coniferous Tree line
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Plant Physiognomy Tree line climate can produce strange tree forms - krummholz Atypical growth pattern resulting from borderline growth conditions - mean annual soil temps. <5-8°C, air temps. ~10°C
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Plant Physiognomy Gradual transition from west to east, grassland to woodland to forest Changes in amount, seasonality of rainfall
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Plant Physiognomy East of Rockies, start with short-grass prairie Low-growing clumps of grass with bare patches between clumps
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Plant Physiognomy Gradual shift from midgrass prairie to tallgrass prairie in Nebraska/Iowa Taller grasses, forbs, more diversity and biomass Follows pattern of increasing rainfall
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Plant Physiognomy Further east - trees appear in places other than along streams Woodlands - dominated by trees, but without a closed canopy (oak savanna)
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Plant Physiognomy Forests appear near Illinois-Indiana border Continue to the east coast
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Plant Physiognomy Seasonality of precipitation (spring and fall) and warmer temperatures increase chance of drought in grasslands
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Plant Physiognomy Mid-, tall-grass prairies experience fire every 3-5 years (too little combustible material in short-grass prairie) Trees can’t survive frequent fires (apical meristems)
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Plant Physiognomy Woodlands appear where fire frequency is low enough to allow trees to grow tall enough to avoid fire Still are more fire-tolerant species
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Plant Physiognomy Precipitation in forests is high enough to keep fire frequency low
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