Lecture 22: Climate Flashcards
-Forcing and Feedback -Natural Variability -Shifting Continent and Tectonics Affect Long-Term Climates -Solar and Orbital Forcing -Milankovitch Cycles
What controls Earth’s climate?
A complex interaction between all the “spheres”, changed and controlled through a myriad of complex forcings and feedbacks.
What is a forcing?
When something causes an imbalance between the absorption of solar radiation and energy emitted by the top the Earth’s atmosphere.
What is a feedback?
The reaction of the climate system to the forcings, which can lead to a change in the forcing that started it. Can be positive or negative.
What is weather?
The state of the atmosphere at any given place and time.
What is climate?
The average state of the weather on time scales of seasons and much more. Often expressed as 30 year averages.
What is a negative feedback?
A feedback that diminish the mechanism of change.
-Ice-albedo feedback
What is a positive feedback?
A feedback that amplify the mechanism of change.
-Water-vapor feedback
What are some external forcings?
- Tectonic
- Orbital
- Solar
- Volcanism
- Anthropogenic changes
What are some of the internal forcings?
- Greenhouse gases
- Aerosols
- Albedo
- Ocean-atmospheric circulation patterns
What is natural variablility?
It refers to how climate has varied through time due to natural external and internal forcings.
What are the two states of the Earth climates?
Greenhouse and Icehouse
What is the quaternary?
The current and most recent of the three periods in the geological time scale.
What is the holocene?
The period that started after the last ice age.
How does tectonic forcing change basic feedback cycles?
- It alters the distribution of land masses/oceans and thus the distribution of surfaces with different heat capacities and albedo.
- It affects global and regional climate patterns
- -Affects weathering rates and thus the concentration of Carbon Dioxide in the atmosphere.
What does solar forcing cause?
A change in the total solar irradiation (TSI) received at the top of the atmosphere.