Exam 2 Flashcards
Condition
Abiotic environment that varies in time and space and to which organisms respond differently.
Components of condition
Temperature, pH, humidity, water flow rate
Resource
Factor that organisms may use up and make less available for others
Performance of Species graph
Species that survive may not be able to grow or reproduce. Species that grow may not be able to reproduce.
Homeotherms
Approximately constant body temperature. “Hot blooded”
Poikilotherms
Variable body temperature. “Cold Blooded”
Endotherms
Heat generated internally
Ectotherms
Heat from environment
A lot of hibernating animals are this
Poikilotherms
Behavioral thermoregulation
Can control body temperature based on behavior
Advantage of Ectothermy
Generally low cost. Plants can put more towards growth than towards thermogenic machinery. Choice of environment limited though
Advantage of Endothermy
Can exploit more environments. High energy cost though
Short wavelengths provide…
More energy
Photosynthetically active radiation (PAR)
Radiation that can be used by plants
Enhanced Greenhouse Effect
Infrared rays get into earth and cannot escape. If at an increased rate then can’t escape atmosphere
El Nino Southern Oscillation (ENSO)
Warm water is sloshed back to South America and cold water is covered, resulting in less nutrient for wildlife, productivity decreases
Red Kangaroo Population during ENSO
Declined. Droughts reduced amount of vegetation kangaroos could eat.
Grasshopper thermoregulation
Change pigment. Increase potential for Hr gain (dark) or Decrease potential for Hr gain (light)
Torpor
State of low metabolic rate and low metabolic temperature
Hibernation
Torpor happening during the winter
Estivation
Torpor happens during the summer
Greenhouse Effect
Atmosphere keeps surface of Earth warm. Gasses absorb infrared radiation emitted by solar heated earth and re-emit most energy back to the earth.
Walker Circulation
Air over warmer Western Pacific rises, flows eastward in the upper atmosphere, then sink over eastern pacific. Air mass then flows westward along southeast trade winds, gradually warming and gathering moisture. Western flowing air eventually joins the rising air in the western pacific. As warm and moist air rises, it forms rain clouds
La Ninas
Periods of lower sea surface temperature and higher than average barometric pressure in the eastern tropical pacific