Long Exam 1 - Individual Genetics Flashcards
Coriolis Effect
Winds in the Northern Hemisphere are deflected to the RIGHT of the direction they travel; reverse for Southern Hemisphere
Upwelling
When cold water deeper in the ocean comes up to replace displaced water at the surface
Why are Deserts dry?
- Cold DRY air sinks at 30degrees N/S
- It absorbs moisture from the ground via water gradient
Why do Tropics always rain?
- Cold moist air from 30degrees belt N/S come to Tropics
- It becomes warm moist air, rising into the upper atmosphere [warm air rises]
- In the cold atmosphere, moist air condenses and precipitates, raining onto the tropics
- Cold dry air following the wind belt, descends at 30 degrees belt N/S repeating the cycle
Which ways do the Polar Easterlies, Westerlies, and Northeast trade winds move towards? [in the northern hemisphere]
- Polar Easterlies: Left
- Westerlies: Right
- Northeast Trade winds: Left
*Their names are where they COME from
Which boundary current carries warm water?
Western Boundary Current: Clockwise in the NH, counterclockwise in the SH. Carries warm water from the equator
O horizon
Organic layer - freshly fallen organic matter, nutrient-rich
A horizon
Mixture of clay, silt sandB
B horizon
largest layer
clay hummus and other materials LEACHED from higher layers
Often plants roots found here
Leaching
Rainfall pulls nutrients into lower layers
C horizon
Weathered plant material
High Constant Temperature
High Constant Rainfall
No Freezing Months
Tropical Rainforests
Tropical Rainforests Flora
Nutrient-poor soil
Plants with long roots
Mycorrhizae
Fungi that help rainforest plants obtain phosphorous from soil; symbiotic relationship with plant roots [they make sugars for the fungi]
High Consistent Temperature
Long wet seasons w/ high peaks
Dry seasons
No Freezing Months
Tropical Dry Forests
Tropical Dry Forest Flora
Plant species are more resilient to dry seasons
Richer, dryer soils = soil erosion
High Temperature
Short wet seasons w/ high peaks
No Freezing Months
Savannah
Savannah Flora
Seldom trees
Soil have low water permeability = bad for trees
Drought associated with dry seasons lead to lightning-causes wildfires
Temperature > Rainfall
Low Rainfall
Sometimes Freezing Months
Desert
Desert Flora
Low plant cover and animal abundance but HIGH biodiversity
Decomposition rates decrease in dryer conditions = low organic matter = nutrients stuck in dead organisms
Summer drought
No Freezing Months
Mediterranean Woodland and Shrubbery
Mediterranean Woodland and Shrubbery Flora
Moderate soil fertility
Trees and shrubs particularly evergreen
High Temperature
High Rainfall [coincide]
Some Freezing Months
Temperate Grassland
Temperate Grassland Flora
Rarely any trees
Nutrient-rich soils = agriculture
Herbaceous vegetation
Temperature < Rainfall
Temperature is Inconsistent
Freezing Months
Boreal Forest
High Consistent Rainfall
Short seasonal drought season [spike down]
Low Temperature
Freezing Months
Coniferous Temperate Forests
High Consistent Rainfall
Low Temperature
Freezing Months
Deciduous Temperate Forests
Temperate Forests Flora
Deciduous = flowering plants [moisture dependent]
Coniferous = cones [resilient to moisture variation]
High biomass production
High soil fertility
Tall Trees
Boreal Forest Flora
Thin acidic soil, low in fertility
Evergreen conifers
High animal density
Freezing Months
Precipitation > Temperature but very low precipitation
Relatively moderate temperature variation
Tundra [seas regulate temperature]
Turnover Time
Time required to completely replace the volume of a water reserve
OCEAN STRUCTURE
Littoral Zone
Oceanic Zone
Littoral Zone: Intertidal Zone / Shallow shoreline
Oceanic Zone: Beyond continental shelf
Humboldt current
Carries cool arctic waters towards Galapagos islands via EBC
5 layers of Oceanic Zone [Oceans ecosystem]
Epipelagic
Mesopelagic
Bathypelagic
Abyssal
Hadal
Benthic
Ocean floor
Pelagic
Above ocean floor
Thermocline
Layer of water through which temperature rapidly changes with depth
Halocline
Layer of water through which salinity rapidly changes with depth
Pycnocline
Layer of water through which density rapidly changes with depth
Thermal Stratification
Water layers are separated by heat as warmer waters become less dense
Advection [Ocean]
Horizontal movement of cold polar waters towards the equator; to replenish nutrients and O2
Bioluminescence
Production and emission of light by organisms; only light apparent past 3,400m
Why are the poles saline during winter but unsaline during summer?
SUMMER: ice caps melt, diluting the polar waters
WINTER: water freezes, leaves behind salts
Where is the highest salinity?
Where is the lowest salinity?
- HIGHEST: SUBTROPICS, where evaporation > precipitation
- LOWEST: TROPICS, where rainfall > water evaporated
Ocean Light
80% absorbed in the first 10m by plankton
Bioluminescence
Ocean Water Movement
Advection
Wind-driven surface currents creates gyres
Deepwater currents causes upwelling
Ocean Salinity
34-36.5 ppt [parts per thousand; 34g of salt in 1000g of water]
Ocean Oxygen
200 ml of O2 per 1000ml air
VS 9ml of O2 per 1000ml water
O2 concentration decreases with depth UNTIL it reaches the pycnocline [LOWEST: decomposition rates highest, breathing by feeders] Below pycnocline, high oxygen levels due to advection.
Ocean Biology
Photosynthetic organisms found in upper epipelagic zone [EUPHOTIC ZONE]
CHEMOSYNTHESIS: occurs near hot springs
Shallow Marine Waters STRUCTURE
3 Reef Categories
- Fringing Reefs [hug shores]
- Barrier Reefs [between open sea and lagoons]
- Coral Atolls [coral inlets built up from submerged islands]
Shallow Marine Waters
LAGOON
a stretch of salt water separated from the sea by a low sandbank or coral reef.
Shallow Marine Waters
INTERTIDAL ZONE 4 CLASSIFICATIONS
- Supratidal Fringe: seldom covered by high tide; sea spray
- Upper Intertidal: covered only during highest tides
- Lower Intertidal: uncovered only during lowest tides
- Subtidal: rarely uncovered