Utilisateur
clilmate, water, nutrients and substrate
long term temperature, preticipattion and wind patterns. determines biome distrobution
they are essential elements for plant growth and their distrobution effects productivity
physical base like soil or rocks. soil types fertility, ph and drainage control what organisms can grow
latitude
at a higher angle, it is a smaller area and more concentrated therefore hotter
at a lower angle, it is spread out ove a alrge area therefore colder
the variation in heat inputs that set up predictable climate zones
1) Shapes biomes, allows us to see predictable distrobution of ecosystems. 2) Controls energy availability, Temperature comes from solar rediation concentration which drives photosynthesis ( areas with higher sunlight, like the equator, supports higher productivity. Colder regions ( poles and high mountains) have shorter growing season=lower productivity. 3) determines species distrobution, every species has a thermal tolerance and temperature range where it can survive and reproduce. also sets boundires for wher organisms can live
the earth's tilt (23.5), which changes the solar input throughout the year
the worldwide movement of air and indirectly water, caused by the uneven heating of the earth's surface by the sun and earth's rotation
the equator gets the most direct solar energy and hot, moist air rises
circulation cells from 0-30 latitude where warm, moist air rises at the equator which causes a heavy rainfall and tropical rainforests, then sinks dry at 30 which creates deserts. ( desending poleward)
circulation cells from 30-60 latitude, driven by intercations between hadley and polar cells producing temperature climates with moderate rainfall, specific season and variable weather
temperature
circulation cells from 60-90 latitude where cold, dry air sinks at the poles which makes cold, low precipitation environments likes tundra and polar deserts
the dominant global wind patterns that are formed by circulation cells and the earth's rotation that continously move air in specific direction.
trade winds, westerlies and polar easterlies
it causes the deflections of winds clockwise (high pressure) in the north hemisphere and counterclockwise (low pressure) in the south hemisphere
global wind patterns, ocean currents and climate regulation.
the equator is faster since it is wider than that the poles
different parts of the globe have different seasonal differences. larger difference with areas that have hot summers and cold winters. smaller differences in coastal/oceanic areas, with more stables and elss seasonal changes
when moist air comes inland from the ocean and hits a mountain range, it has no choice but to rise up the slope
The side facing the ocean/wind. As the air rises, it expands and cools, cooler air cant hold as much moistures so water vapor condenses, producing clouds and precipitation (rain or snow) which results in a wet, lush environment like a temperate rain forest
The downwind, away from the ocean. After the air loses its moisture, it descends on the other side of the mountain. descending air warms and becomes very dry. resulting in arid conditions (rain shadow desert)
biomes are large scale ecological communites were climate ( temperature and precipitation) determines the vegetation, which then determine the species that can survive there.
the rate at which plants convert solar energy into chemical energy through photosynthesis. It determines the base of foodwebs and how much energy is available for higher trophic levels
the energy that's left after plants use some of the energy for respiratin. represents the energy available for herbivores and decomposers.
the biomass and more species are supported
Temperature, water and radiation
warmer climates mean higher ensymatic activity and photosynthesis. Lower temperatures (tundra) shorten growing seasons and extreme heat can cause droughts/stress
it is essential for photosythesis and nutrient transport in plants. higher rainfall = lush vegetation (rainforests). Low rainfall = deserts with very low productivity. water availability interacts with temperature. (hot + dry = strong limitations)
more sunlight = more energy for photosythesis. Cloud cover/ high altitudes reduce solar input and strongy effects productivity.
High NPP= dense plant growth, high biomass, more resources for herbivores and canivores = higher biodiversity (tropics). Low NPP= spares vegetation = limited resources, fewer species are supported (deserts, tundras and polar regions)
The global mouvement of ocean water diversity by temperature and salinity differences.
it regualtes global climate by transporting heat and circulates nutrients and oxygen, supporting marine ecosystems
because warming and melting ice can reduce salinity and density which slows currents and impacts climate
1) light availability, algae and phytoplankton can only live near the surface, where sunlight hits so they can photosynthesis. deep water has no light therefore no photosynthesis can occur. 2) Nutrients, high productivity near coast and upwelling zones where currents bring nutrient rich water to the surface.
poles have strong upwelling + seasonal sunlight whihc produces high productivity in the summer. Equator has lots of sunlight, but productivity is limited beacuse nutrients are scares since in tropical regions they get taken by plants for NPP, leaving very little available in the water column
summarize climatic info using standardized structure
temperature on left vertical axis, precipitation on right vertical axis, all 12 months on bottom horazontal axis. 10C to 20mm precipitation plotting. precipitatin blue (usually higher than temp) and temp red.
nutrients in soil determine ecosystem functions. what plants grow, what animals are supported and overll biodiversity.
rain and temperature control soil development. more precipiation= more nutrients are washed away.
wet tropics (oxisols)
rich and fertile soil good for agriculture (prairies and grassland)
low organic matter and limited productivity. (deserts)
agriculture exports nutrients from soil and causes shifting cultivation
when land is burned, nutrients temporarily return to the soil, which allows crops to grow, but after repeated use nutrients are exhausted and land needs to be left to recover
local soil and water conditions make ecological communities
the direction a slope faces (aspect) changes how sunlight is exposed and affects temperature and moisture
