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HIPPO
habitat destruction invasive species population pollution overharvesting
temp in troposphere
cools as it rises because fewer molecules
temp in stratosphere
warms as it rises because exothermic reaction with UVb and oxygen
Temp in mesosphere
cools as it rises because not enough oxygen
temp in thermosphere
warms as it rises because of xrays and gamma rays 4deg/1000m lapse rate
atmosphere layers
troposphere stratosphere mesosphere thermosphere
main wind cells
Hadley Ferrel - westerlies Polar - easterlies
moist adiabatic lapse rate dry adiabatic lapse rate
6 degrees/1000m 10deg/1000m
physiological adaptations to heat
conserve water reduce heat reduce water loss
physiological adaptions to cold
small, dense pubescence - insulation succulent (heat capacity) reflective - parabolic to flower
Freshwater systems
lotic and lentic
lotic system
unidirectional continuous physical change river continuum concept spatiotemporal heterogeneity species response
two energy input types
autochthonous allochthonous
5 factors of continuous change in river
slope volume oxygen content temperature energy input
energy input at headwaters of river
mostly autochthonous from surrounding trees, consumed by shredders Oxygen high, temp low, PS/R <1
spatiotemporal heterogeneity
five factors never the same at any two points. energy inputs lead to this. no single river bioms
species response to RCC
relative abundance changes, no single river biome
Lentic system
light absorption spatiotemporal heterogeneity species response
light absorption in lentic system
reds absorbed at top of ocean, then blue red and blue absorbed in lake, green and yellow left
spatial zones in lentic system
euphotic: littoral and limnetic profundal benthic
euphotic
zones with light
littoral
shoreline trophic levels, periphyton eaten by grazers -> fish -> piscivore
limnetic
pelagic - not near shore 4 trophic levels (phyoplankton, zooplankton, fish, pescivore)
compensation point
where respiration = photosynthesis