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Weather vs Climate Example
Weather - severe thunderstorm/hurricane
Climate - An upward trend over the 30-year average of the frequency of thunderstorms
Weather vs Climate
Weather - what is happening now
Climate - Recorded patterns over decades
Climate Change is always caused by humans (T/F)
False
The Greenhouse Effect
How earth traps heat near the surface, this is don by converting the high energy solar radiation into IR and heat, the lower energy radiation cannot escape
Greenhouse Gases (Top 5)
•Carbon Dioxide (CO2)
•Nitrous Oxide (N2O)
•Methane (CH4)
•Fluorinated Gases (F-gases) (always anthropogenic)
•Water Vapor (not anthropogenic)
Earth's Gas Composition
78% N2
21% O2
.9% Argon
.1% Trace Elements
What Makes A GHG a GHG?
Certain gases absorb IR
•Unless at 0 K, all molecules are constantly vibrating
•"the wiggles"
•Stretching and Bending
•When they do this, IR-active molecules will have a change in dipole moment that allows absorption of IR
Why do we talk about CO2
largely because it is the GHG in the highest proportion in our atmosphere. But, other molecules are capable of absorbing far more IR and it comes down to their structures.
Carbon Pools
Where Carbon is Stored
•Rocks / Fossil Fuels
•Soils
•Atmosphere
•Biosphere (Anything alive)
Ocean (Surface and Deep Ocean often considered separately)
Processes/Flux
How carbon moves between pools
•Photosynthesis
• Respiration
• Soil Respiration
•Combustion
•Vulcanism
• Decomposition
• Diffusion
•Sedimentation
GWP
Global Warming Potential
GHG's GWPs
•Carbon Dioxide: 1 GWP
•Nitrous Oxide: ~300 GWP
•Methane: ~30 GWP
•Fluorinated Gases: Average ~ 5000 GWP
N2O vs NOx
•NOx is an indirect greenhouse gas
•NOx produces ozone (O3)
NOx has a 100 year-GWP = 10
Ozone
•Ozone absorbs UV-B
•Causes sunburn/DNA damage in humans
•Ozone in the troposphere acts as a potent GHG
•~1000 GWP
•Ozone is incredibly short lived
•Half-Life: 10-60 min in air
Ozone does more good than harm
Climate Impact
GWP x quantity of gas
Measures the overall contribution to Climate Change
CO2 is...
The most impactful, 64%
Carbon Cycle
How carbon changes and moves with Pools and Fluxes (Processes)
A vast majority of anthropogenic CO2 emissions come from...
the burning of fossil fuels
Feedbacks
agents of stability or rapid change
Negative Feedbacks
Promote changes that lead back toward equilibrium
"overshoot, undershoot, overshoot, undershoot"
Ex. Predator/ Prey Dynamics

Positive Feedbacks
Systems that promote further change toward an extreme.
Amplification of a stimulus
"build, build, build, CRASH"
Ex. Labor , Avalanche

Albedo
Ability of a surface to reflect light
Albedo Feedback
As atmospheric temperatures rise, ocean water warms, melting sea ice. This exposes low-albedo seawater, which absorbs more sunlight, further warming the ocean and accelerating ice melt in a growing cycle.
Water Vapor Feedback
Rising GHGs warm the air, increasing evaporation. Warmer air holds more water vapor, a greenhouse gas that traps heat, further boosting evaporation and warming in a cycle.
water cycle
1)Condensation - water vapor in the air condenses into clouds
2)Precipitation - water in clouds falls back to earth as rain, snow, sleet, etc.
3)Transpiration- water lost from plants into the atmosphere. Can be thought of as evaporation from plants through their stomata
4)Evaporation - liquid water that is converted into water vapor from the surface of lakes and oceans and soil. Sometimes this is combined with transpiration to identify the amount of water vapor put into the air as evapotranspiration
What are the effects of climate change on the water cycle?
•More episodic precip (less frequent)
•More intense (more precip in heavy rain events)
•Increasing Drought and Flooding
•Shifting weather patterns and stronger storms
•Less Snow
Permafrost Feedback
The Arctic warms faster than the rest of the world due to permafrost and albedo feedback. Permafrost, like a frozen soil popsicle, traps carbon but is now thawing, releasing greenhouse gases. Most decomposition here is anaerobic, producing methane—a far more potent GHG than CO2, with each pound of methane equating to 28 pounds of CO2, accelerating warming.
Migration
Moving across the landscape (different than seasonal migration)
Climate Envelope
The set of environmental/climatic conditions that an organism requires in order to survive
When envelopes move, species will try to move with them if they can.
Plants...
Struggle to migrate at the rate needed to stay in their envelope
Phenology
The timing of seasonal changes in plants and animals ex. Flowering, migration, calving, molting, etc.
The result of earlier spring / longer growing season
Phenological Mismatch
When the timing of events for interacting species no longer co-occur
If something can't migrate
Adapt/Evolve or go extinct
Kelp Forest
An aquatic ecosystem dominated by giant kelp (Macrocystis) which is a brown algae. They provide important food and habitat for many species.
Kelp are macroalgae
Have blades that that do most of the photosynthesis and vascular tissue, but they don't have stomata and gas exchange is through diffusion/active transport
kelp forests' complexity/info
far more complex than most other marine ecosystems
Extremely High Vertical Complexity
High Horizontal Complexity
High Resistance
High Resilence
High O2 content, and cold
Best Marine Ecosystems
are NOT at the equator
Temperature and dissolved oxygen
Are inverses of each other

Temperature has a strong impact on..
All Marine Ecosystems
How have Kelp Forests done in recent times
Drastically Declined
Regulator
keeps internal environment constant regardless of external environment
Conformer
internal environment matches external environment
Thermoregulation
•Temperature Control
-Includes special enzyme functions,
-must be careful of denaturation by heat
•Energetics (Confromer pro)
Thermoconformers don't need to spend energy regulating their internal temperatures >>> put that energy into other activities (finding food)
•Biochemistry (Regulator Pro)
Thermoregulators are always operating at biochemical optimum
Migration (Conformer Con)
•Thermoconformers may need to migrate to stay within an ideal temperature
brumination
similar to torpor/hibernation but the alligators will move when it gets warmer, low MBR
Types of Thermoregulation
Behavioral: Actions / decisions
Physiological: Internal changes (not visible)
Morphological: External characteristics
Strategies to Increase internal heat
Blubber
Thick Fur
Vasoconstriction
Countercurrent Exchange
Dormancy (Hibernation)
Body Positioning
Basking
Metabolism (Thermogenesis)
Strategies to decrease internal heat
Sweating
Panting
Vasodilation
Surface Area increases
Wallowing (mud, water, etc)
Body Positioning
Dormancy (Estivation)
Metabolism
•All of the chemical reactions in the body
1.Energy Conversion
2.Building Block Synthesis
3.Waste Elimination
Includes Anabolism - Synthesis
Includes Catabolism - Degradation
How do humans thermoregulate
We use metabolism to influence our temperature, metabolic rate increases as temperatures go up and down
Thermoneutral Zone
The temp range in which metabolic rate does not need to rise to maintain body temp
Respiration rate
how fast we burn calories
Homeotherm
•Have a very small range of tolerable internal temps
Poikilotherm
•Have a wide tolerable range of internal temperatures
•No permanent harm (though biochemical processes will speed up or slow down with temp)
Endotherm
- internal temp can be controlled by altering metabolic rate (all birds and mammals)
Ectotherm
body temperature cannot be controlled with metabolism (reptiles, amphibians, fish and invertebrates)
Main ideas from metabolic demands
Big animals require more energy (more biomass to move and maintain, etc.).
Between endotherms and ectotherms of a similar size, endotherms have higher BMRs.
Endotherms vs Exotherms Metabolism
Endotherms burn more calories in an effort to maintain their internal temperatures and to counteract heat loss to the environment. Ectotherms rely on the external environment to maintain temperature, so no calorie expenditure is required to maintain heat.
Larger animals TOTAL energy requirements
animals have more cells that need energy, they have to move more weight around. Higher total energy requirements
higher per kg requirements?
Small organisms, they lose more heat bc of the higher surface area to volume ratio, so they need more food
Marine vs Terrestrial
Marine mammals have higher metabolic requirements than terrestrial mammals
How do sea otters thermoregulate
THICK fur
Thermogenesis
Skips ATP and generates heat
Needs high amounts of food
Homeostasis
A dynamic equilibrium which is actively regulated to maintain a variable (the health of an animal) at a constant level
Osmoregulation
The ability to regulate the amount of solute internally relative to external solute
Osmoconformer
does not regulate the amount of solute internally relative to external solute
Is osmoregulation constant?
No, it depends on the environvemt, and salinity of water
Cellular respiration
transforms the energy in organic molecules into ATP and heat
Energy is...
Stored inside of bonds as potential energy
Energy flows through biological systems according to
the laws of thermodynamics
1. Energy can be transferred and transformed, but not created or destroyed
2. Every energy transfer or transformation increases the entropy (disorder) of the universe
Only some of the energy that is released is useful
Most is "lost" as heat or waste
Food Webs
Energy diagrams that show how energy flows through an ecosystem based on what eats what, all organisms are not equal

Trophic level
where an organism is in the food chain
Autotrophs Carbon Source
Inorganic C (CO2)
Heterotrophs Carbon Source
Organic C (C & H) (Anything alive or used to be alive)
How much energy is retained by each trophic level
10%
Energy goes to
Feces
Growth
Cellular Respiration
Plankton
Anything that drifts with tides and currents
Often microscopic
What are the autotrophs in the kelp forest ecosystem?
phytoplankton
Phytoplankton
•"Plant plankton"
•Photosynthetic microorganisms/algae
•Contribute ½ of the world's oxygen
Zooplankton
•Usually just small invertebrates
•Eat phytoplankton or other zooplankton
The difference between choosing prey
ENERGY GAINED - ENERGY SPENT
Some have more calories, but take more energy to obtain
OPTIMAL FORAGING THEORY
Organisms use foraging strategies that maximize energy gain
Prey Switching
switching to the next best prey item when a preferred item becomes rare
Sea Urchins
•Invertebrates
•Related to sea stars (echinoderms)
•Mostly Herbivores
•Spines for protection
•Kelp is primary food source when available
Destroy Kelp forests if not regulated
Trophic cascade
when changes at one trophic level have dramatic effects throughout a food web
Keystone Species
an organism with an outsized influence relative to its abundance
Apex Predator
an organism at the top of the food chain
Why are Kelp Forests better than Urchin Barrens
•Carbon sequestration
•Vertical complexity
•Biodiversity
•Ecosystem stability
•Ecologically important Juvenile fish habitat
Alternative Stable States
•Ecosystems can have multiple stable modes that are difficult to transition out of.
It can be very difficult for the ball to move back to the original trough and requires another kind of very large disruption to do it.

K
Carrying Capacity
What are 2 pieces of evidence from the Estes et al. paper that implicate orcas?
•A small # of orcas could greatly decrease otter pop
•Only otter loss in open ocean
•No washed up sea otters
•No relocation of sea otters
•Increased orca attack sightings
pollutants that accumulate in organisms over time
•Metals/Metalloid*
•Hg, Pb, Cd, Cr, As*
•POP's - Persistent Organic Pollutants
•(PFAS, PCBs, DDT)
•Stored in fatty tissue
•passed on through blood and milk
Toxin accumulation causes excess mortality in 2 ways:
•Trophic level
•Age
Bioaccumulation
Toxins build up in an individual as it ages.
Biomagnification
Toxin concentrations increase as you move up through trophic levels
Can both happen at once
Yes, ex. Old Large Tuna (Apex predator trophic level, and by age)
persistent chemicals that biomagnify
Hg, Pb, Cd, As*, PCB's and DDT
Ocean Acidification (OA)
•Ocean water is usually basic, so it's becoming less basic (more acidic)
•More CO2 in atm. = more CO2 in ocean (diffusion)
•A result of increasing atmospheric CO2, not climate change directly