Review:
Seasonal cycles of light, nutrients, and chlorophyll for the temperature North Atlantic
Light: dark in winter and fall, lighter in summer and spring
Nutrients: high in winter and fall due to less dense waters making it easy for mixed layer depth, spring and summer are warmer waters so less nutrient rich because more stratification
Chlorophyll: low in winter and fall because less light means less photosynthesis; on the other hand, high in summer and spring due to abundance of light but in summer, nutrients are depleted so it declines
Differences between El Nino and La Nina:
El Nino produces warmer waters in the eastern pacific and trade winds are weakened; more rainfall in eastern pacific but droughts in the west; leads to decreased productivity and fish die
La nina produces colder waters and trade winds are stronger; there is less rain in the eastern pacific but more rain in the west; increase in productivity
Colder = more chlorophyll since mixed deep layer is deepened
Observed anthropogenic climate change and future projections
World is getting warmer due to global warming
Increases are greater over land and polar zones; tend to be weaker in the ocean since the ocean modifies these changes
Warming and salinity changes lead to increased stratification and this causes a decrease in nutrient delivery
With increased stratification, there is less ventilation (less oxygen) in the ocean surface because everything is separated
Hydrology is changing due to runoff patterns shifting
Mountains are accumulating snow but due to the warming of the earth, it melts earlier/faster causing runoff
Oceans are getting warmer so abnormal blooms are occurring causing economic consequences (can be poisonous to aquatic life)
Oceans are becoming more acidic, certain organisms cannot handle the acidity such as pterpod
Greenhouse effect: atmosphere is transparent and trapping the radiation being emitted from earth (longer) so is warms the earth in general
Sunlight that comes in is either absorbed by the surface or reflected by clouds
Some absorbed by atmosphere and gets trapped, making climate increase
Arctic ice is melting quickly due to the warming of the earth
Ice is much thinner and melts almost entirely during summer
Causes the albedo to decrease since the surface is less reflective with less ice
Positive feedback as the ice melts and creates a dark surface that absorbs more heat and leads to more things melting
Increase in sea level because when you warm water, it expands
There is not necessarily an increase of water being added because the ice was already there, just not melted
Rainfall is hard to determine, lack data, fairly new field
Some areas are wetter and received more rain but others did not
Hard to tell because data is not conclusive with everything
Extreme rainfall and flood events are more likely to occur in warmer climates
Future predictions utilize a climate model that can predict the climate over a decade
Newer models are now made that have higher spatial resolution
Represent more factors chemically, physically, and environmentally
Includes the biology and ecology of land.water
Can they be trusted?- with considerable confidence since the models are based off of accepted physical principles and they have worked in the past
Sources of uncertainty: scale and resolution; imperfect understandings of natural processes; natural climate variability; unknown future emissions due to human activities
Impacts of climate change
On humans and society:
Water supply: we get water from mountains and since climate is warmer, the ice is melting sooner and more runoff
Agriculture: increase in temperature means crops must be adapted to be able to handle the warmer climate or else humans have no food
Human health: heat waves have killed thousands of people
Infrastructure: sea levels are rising due to the water getting warmer, people need to be more mindful when building homes and buildings near oceans
On marine ecosystems?
How do organisms respond to climate change?
Move in space or time, change behavior, acclimate through physiology, evolve, change in fitness and abundance
Warming has increased stratification so there are less nutrients at the surface for phytoplankton
Tropics and mid-latitudes (nutrient limited): less mixing and lower supply of nutrients so there are less plankton at the surface/in general
High latitudes (light limited): less mixing but increase in plankton at the surface to get all the light they can
In light limited, high latitude regions of the ocean, anthropogenic climate change is projected to: increase net primary productivity because the plankton are forced to come to the surface due to the lack of nutrient delivery
Biomass of diatoms will decrease since there is less nutrients due to increased stratification; thus, smaller phytoplankton will become dominant
Export production: flux of particles out of the euphotic zone (uppermost surface where light penetrates)
Decrease globally but increases in high latitude where phytoplankton growth is light/temperature limited
Decreases because warmer waters = more stratified
But areas with limited light are colder so upwelling can occur to bring the nutrients up
Biological pump may be weakened: co2 levels increase and further warm climate since the plankton cannot take it in
Subpolar: stratification increases, nutrient delivery to surface decreases, primary production increases, export production increases
Subtropics: stratification increases, nutrient delivery to surface deceases, primary production decreases, export production decreases
increasing CO2 levels could hinder growth of some phytoplankton but help others
Some phytoplankton blooms are occurring earlier than expected and they are moving/out of range