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Ecology 2

QuestionAnswer
Water Vapor Density Amount of water vapor per unit volume of air
Saturation Water Vapor Density Maximum amount of water vapor air can hold. Increases as temperature increases.
High Relative Humidity Air contains more water -> less evaporation
Low Relative Humidity Air is drier -> more evaporation
When RH is less than 98%, atmospheric water potential is very low
Two major challenges for terrestrial organisms 1. Evaporative water loss 2. Limited access to replacement water
Evaporation cools organisms, but it also causes water loss
Freshwater -Very low osmolarity -Organisms in hypotonic environment
Seawater -High osmolarity Organisms in hypertonic environment
Terrestrial challenges Prevent water loss
Freshwater challenges Prevent excess water from entering
Marine challenges Prevent water loss to salty environment
Lichens Poikilohydric (water content changes with environmental conditions). Can tolerate periods of drying.
Factors affecting microclimates: Altitude Higher altitude-> lower temperature
Factors affecting microclimates: Aspect Direction a SLOPE faces. changes the amount of sunlight received.
Factors affecting microclimates: Albedo Dark SURFACES-> absorb more energy. Proportion of incoming light that is reflected. Snow->high albedo->reflects more energy
Water potential Water moves from high water potential to low water potential
Pure water: ψ = 0 MPa
Solute potential (ψsolute) Dissolved substances lower water potential. more solute->more negative
Matric potential (ψmatric) Water attracted to surfaces through adhesion/cohesion.
Pressure potential (ψpressure) In plants, negative pressure can result from transpiration.
Root development Root systems often reflect water availability. Deep roots are advantageous when water is deeper in the soil.
Morphological adaptations: Reduced leaf area → less surface for water loss
Morphological adaptations: Deep roots→ access deeper water
Morphological adaptations: Water storage → stores water for dry periods
Morphological adaptations: Thick leaves → reduce water loss
Morphological adaptations: Suberization → Suberin creates a waterproof barrier
Morphological adaptations: Few stomata → reduces water loss
Succulence Increased osmolarity helps retain water in tissues.
C3 Plants (least specialized for hot/dry conditions) Hot conditions -> increased evaporation -> stomata close. Closing stomata causes: decrease of co2 and photosynthesis. increase of o2 and photorespiration.
C4 Plants (Spatial separation) Adaptation to hot, dry conditions. Can partially close stomata to conserve water. CO2 is initially captured in mesophyll cells. Calvin cycle occurs in bundle-sheath cells.
CAM Plants at night (temporal separation) Stomata open, CO2 enters, CO2 is stored as organic acids.
CAM Plants during the day (temporal separation) Stomata close, CO2 is released from organic acids, CO2 enters the calvin cycle.
Plants can avoid drought stress by: *Synchronizing growth with we periods *Drought deciduousness (dropping leaves during drought) *Desert annuals (complete life cycle during wet periods) *Dormancy (temporarily stop growth/activity)
Metabolic water produced during cellular respiration
More water vapor in air-> and why? Less evaporation. Smaller water vapor gradient between organism and environment
High Vapor Pressure Deficit Dry air-> more evaporation
Low Vapor Pressure Deficit Humid air-> less evaporation
Water conservation Behavior, anatomy, kidney adaptations
Nephron Main functional structure of the kidney.
Loop of Henle: Descending limb Permeable to water, water leaves the tubule, urine becomes more concentrated.
Loop of Henle: Ascending limb Not permeable to water, NaCl (salt) leaves the tubule->helps create the kidney's osmotic gradient.
Collecting duct Water is reabsorbed as fluid moves toward the inner kidney. Produces highly concentrated urine.
Kangaroo Rat Maximizes kidney's osmotic gradient. Produces extremely concentrated urine and minimizes water loss.
Waste: Ammonia Most toxic, most water needed
Waste: Urea Intermediate toxicity, moderate water needed
Waste: Uric acid Least toxic, least water needed
General Water-Conservation Strategies in Terrestrial Animals Waterproof outer coverings Concentrated urine Dry/concentrated feces Behavioral adaptations → nocturnal activity, sheltering, etc.
Isosmotic Internal and external solute concentrations are equal.
Osmoconformer Internal water/solute concentration changes with the environment.
Osmoregulators Maintains internal water and solute concentrations within narrow limits. -Actively controls despite outside salinity
Hyperosmotic Environment has higher solute concentration than body fluids.
Hypoosmotic Environment has lower solute concentration than body fluids.
Marine Fish Hyperosmotic relative to their body fluids. Marine = drink + dump salt
Freshwater Fish Hypoosmotic relative to their body fluids. Dump water + grab salt
Osmoconformers Internal salt/water concentration changes with the surrounding environment. (marine invertebrates)
Stenohaline Steno= narrow Tolerates a narrow range of salinity
Euryhaline Eury=broad Tolerates a broad range of salinities.
Weather Atmospheric conditions over a short time. Small geographic area. What is happening now
Climate Long-term patterns of temperature and precipitation Considered over many years, larger regions. What actually happens.
Altitudinal patterns Higher altitude = different temperature/moisture = different vegetation
Adiabatic cooling Cooling occurs because air expands as pressure decreases
Higher altitude... lower atmospheric pressure, air expands, molecules have larger volume, temperature decreases.
Lapse rate average temp decrease= 6.4°C per km Depends on moisture
Earth's obliquity Rotational axis= 23.4° Axis is NOT perpendicular to earth's orbital plane around sun.
Equator Sunlight strikes Earth more directly. Energy concentrated over a smaller area -> warmer.
Poles Sunlight strikes at a lower angle. Same energy is spread over a larger area -> colder.
Two effects of sunlight angle: Projection effect Higher altitudes, sunlight is spread over a larger surface area
Two effects of sunlight angle: Absorption effect Sunlight travels through more atmosphere at lower angles. More energy is absorbed/scattered before reaching Earth's surface. Less energy reaches surface.
Seasons: Earth's tilt causes solar radition. Tilt is 23.4°
True or false: Seasons are primarily caused by Earth's distance from the Sun. FALSE. Earth's tilt is.
Five atmospheric layers: Troposphere Bottom layer. Where weather occurs. Temperature decreases with altitude.
Five atmospheric layers: Tropopause Boundary between troposphere and stratosphere
Five atmospheric layers: Stratosphere Drier and less dense. Temperature increases with altitude. Contains ozone layer that blocks harmful UV radiation.
Five atmospheric layers: Mesosphere Low air pressure, temperature decreases with altitude.
Five atmospheric layers: Thermosphere Top atmospheric layer, extremely thin air.
Hadley Cell
Created by: Brookelol
 

 



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