Week 3 Flashcards
(29 cards)
The climate is always ____
Changing!
Quaternary epoch:
past 2.5 million years
Pleistocene:
Ice age part of the quaternary
Holocene:
last 10,000 years
Anthropocene:
Since 1950
How do we measure recent climate change?
temp anomaly
what is a temp anomaly?
he difference between an observed temperature and a reference (or baseline) temperature.
Why do we use temp anomalies?
track climate change.
help compare temperatures across different regions and times
The cryosphere - glacier length
remained relatively stable until 1850 (end of ice-age period) at this point the glaciers started to receede
Lost sea ice leads to a change in _____ which leads to a _______
albedo
positive feedback
What are we losing that is changing albedo and more solar energy is being absorbed?
we are losing the snow cover
is average global sea temperature increasing or decreasing
increasing
What station has the longest instrumental climate record in Canada?
Toronto
what is the longest instrumntal climate record in the world?
Central england temperature record
How do we know about climate 1-2000 years ago
Proxy data
Paleoclimatology:
reconstruction of past climates using proxy data
Stratigraphic records
ice cores
ocean and lake sediments
historical documentary data
paintings
travel logs etc
Biological records:
tree rings
corals
Use of proxy records of climate depend on both:
time span of record
resolution of record
What is proxy data:
preserved physical/chemical/biolgical charecteristics that can be used to iinterperet or reconstruct past climate conditions
e.g., tree rings, ice cores, sediments etc.
Historical data (proxy data)
observations of weather and climate conditions
e.g., log, travelers diaries etc.
What can you tell from a tree ring:
seasonal climate regimes results in the formation of annual growth bands
Autochthonous lake sediments:
inputs originate within the lake itself not transported in
(e.g., aquatic plant material, organisms etc.)