Week 3 Flashcards

(29 cards)

1
Q

The climate is always ____

A

Changing!

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2
Q

Quaternary epoch:

A

past 2.5 million years

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3
Q

Pleistocene:

A

Ice age part of the quaternary

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4
Q

Holocene:

A

last 10,000 years

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5
Q

Anthropocene:

A

Since 1950

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6
Q

How do we measure recent climate change?

A

temp anomaly

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7
Q

what is a temp anomaly?

A

he difference between an observed temperature and a reference (or baseline) temperature.

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8
Q

Why do we use temp anomalies?

A

track climate change.
help compare temperatures across different regions and times

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9
Q

The cryosphere - glacier length

A

remained relatively stable until 1850 (end of ice-age period) at this point the glaciers started to receede

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10
Q

Lost sea ice leads to a change in _____ which leads to a _______

A

albedo
positive feedback

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11
Q

What are we losing that is changing albedo and more solar energy is being absorbed?

A

we are losing the snow cover

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12
Q

is average global sea temperature increasing or decreasing

A

increasing

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13
Q

What station has the longest instrumental climate record in Canada?

A

Toronto

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14
Q

what is the longest instrumntal climate record in the world?

A

Central england temperature record

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15
Q

How do we know about climate 1-2000 years ago

A

Proxy data

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16
Q

Paleoclimatology:

A

reconstruction of past climates using proxy data

17
Q

Stratigraphic records

A

ice cores
ocean and lake sediments

18
Q

historical documentary data

A

paintings
travel logs etc

19
Q

Biological records:

A

tree rings
corals

20
Q

Use of proxy records of climate depend on both:

A

time span of record
resolution of record

21
Q

What is proxy data:

A

preserved physical/chemical/biolgical charecteristics that can be used to iinterperet or reconstruct past climate conditions
e.g., tree rings, ice cores, sediments etc.

22
Q

Historical data (proxy data)

A

observations of weather and climate conditions
e.g., log, travelers diaries etc.

23
Q

What can you tell from a tree ring:

A

seasonal climate regimes results in the formation of annual growth bands

24
Q

Autochthonous lake sediments:

A

inputs originate within the lake itself not transported in
(e.g., aquatic plant material, organisms etc.)

25
Allochthonous lake sediments:
inputs originate outside the lake examples: wind blown soil terrestrial plants terestrial organisms
26
Where is there an ice sheet drill project
greenland
27
Ice core basics:
Records of accumulation can be obtained from the thickness of annual ice layers - impurities in the ice give information about atmospheric circulation and land surface
28
Ice core layers:
young and shallow snow at top older and deeper snow is compacted further at the bottom of the core: rocks, sand etc.
29
Marine sediments:
- long cores drilled by specially equipped ships - isotopes in shells can reveal temp and ice volume - granular debris from land can indicate icebergs breaking off