Lecture 3 - Feedbacks in Global Systems Flashcards

1
Q

positive coupling

A

positively, directly correlated

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
2
Q

negative coupling

A

negatively, inversely correlated

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
3
Q

negative feedback loop

A

negatively and reciprocally correlated

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
4
Q

albedo

A
reflectivity of a surface, the fraction of total sunlight reflected from a surface
ex.) grass 0.2 - 0.3
forest 0.05 - 0.1
snow 0.8 - 0.9
thick cloud 0.7 - 0.8
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
5
Q

example of a positive feedback system with positive and negative couplings

A

global mean temp, continental snow and ice cover, planetary albedo

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
6
Q

example of a negative feedback loop

A

predator and prey populations

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
7
Q

stable equilibrium state

A

ball in a valley between two hills, can withstand some disturbance and the ball will fall back down the hill/return to the mean

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
8
Q

unstable equilibrium state

A

ball on top of a hill

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
9
Q

James Lovelock

A
  • atmospheric chemist at NASA
  • Why has Earth‟s surface temperature remained in steady state for 3.6 billion yrs, while solar radiation has increased by 25%?
  • Gaia Hypothesis
  • Daisy World
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
10
Q

Gaia Hypothesis

A

Like an organism, the Earth is self-regulating/homeostasis

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
11
Q

Daisy World

A
  • Planet imagined to test Gaia Hypothesis
  • daisies affect (lower) surface temperature because the reflect the light
  • temp and photosynthesis
How well did you know this?
1
Not at all
2
3
4
5
Perfectly