climate change Flashcards
(44 cards)
what EVIDENCE is there of climate change? (11 pieces)
- ice cores
- pollen analysis
- sea level change
- historical records
- dendrochronology
- retreating glaciers
- weather records
- polar ice melt
- ecosystem changes
- sea- floor sediments
- fossils
explain ICE CORES
extraction of ice cores which contain trapped bubbles of gas which represent what the gas composition of the atmosphere was like at that time
can be dated to show how atmosphere has changed overtime- can go back approx. 1 mil years
explain POLLEN ANALYSIS
pollen is preserved in sediment- can identify past vegetation types
if pollen is found similar to todays plants, it indicates a similar climate when this pollen was produced
explain SEA LEVEL CHANGE
volume of water stored as ice changes overtime indicated temps changes. e.g. raised beaches show past sea levels (emergent so formed by higher sea levels)
can be dated to show when warmer period was (less water stored as ice)
examples of HISTORICAL RECORDS
DOOMSDAY BOOK- 11th century- record of what farmers grew
painting of THE FROST FAIR IN LONDON- 17th century
explain DENDROCHRONOLOGY
new tree ring every year- thicker ring in warmer+ wetter conditions
can date it to see what climate was like each year (up to 10,000 years ago)
explain RETREATING GLACIERS
rocks deposited by glaciers indicate the size it was+ how far it extended. can be dated to show when they were deposited
distant from current glacier shows climate change e.g. is deposited rocks are far away then temperatures have increased within that period of time
explain WEATHER RECORDS
details of weather conditions consistently collected since 1861- can show detailed climate change over short period of time they’ve been collected
explain POLAR ICE MELT
reduction of ice at both poles- changes in extent of polar ice shows changes in climatic factors effecting them (more melting means increasing temps)
explain ECOSYSTEM CHANGES
changes in temp affect availability of food+ shelter- affects what species live in an area
scientists can use changes in how species are distributed to indicate changes in the climate
explain SEA FLOOR SEDIMENTS
microfossils called foraminifera accumulate in sea floor sediments- can be used to reconstruct past climates as chemical composition of foraminifera shells indicates ocean temps in which they formed
explain FOSSILS
plants+ animals require specific environmental conditions to thrive e.g. coral reefs are sensitive to temperature and water depth
Plant fossils, particularly those of certain species (like palms, cycads, and ferns), can indicate past climate conditions. The distribution of these plants in the fossil record can suggest warmer or cooler climates compared to modern-day locations.
For example, finding fossilized palm trees suggests a warmer, tropical climate.
What are 6 NATURAL FORCINGS of CLIMATE CHANGE?
- milankovich cycles- eccentricity, precession, obliquity
- volcanic eruptions
- meteor impacts
- solar output
- plate tectonics
- natural atmospheric greenhouse gases (CO2)
Which NATURAL FORCINGS of CLINATE CHANGE are INTERNAL?
- volcanic eruptions
- meteor impacts
- plate tectonics
- natural atmospheric greenhouse gases
Which NATURAL FORCINGS of CLIMATE CHANGE are EXTERNAL?
- Milankovich cycles- eccentricity, precession, obliquity
- solar output/ sun spots
Explain ECCENTRICY (stretch)
ORBIT around sun changes from almost perfect circle to ELLIPSE and back again roughly every 96,000 years- changes DISTANCE FROM SUN TO EARTH so AMOUNT OF ENERGY earth relieves changes (at diff times of year)
Currently elliptical orbit
Explain OBLIQUITY (tilt)
Earth TILTS ON AXIS as orbits sun (currently 23.5°) - changes between 21.8 and 24.4 over 41,000 year cycle
Changes AMOUNT OF ENERGY that diff lattitudes receives, changing global climate. Greater tilt (24.4°) means areas receiving lots of solar energy e.g. tropics will be larger, whereas generate zones beyond tropics will be smaller.
Explain PRECESSION (wobble)
AXIS of Earth WOBBLES on 22,000 year cycle
Earth closest to sun in Jan so winter in northern hemisphere is mild and summer is cool (influences INTENSITY and TIMING of SEASONAL CONTRASTS
How do PLATE TECONICS influence CLIMATE CHANGE?
Plate tectonics+ SEA FLOOR SPREADING- distribution of continents has changed
Scale of changes impact climate- LARGE CONTINENTS across HIGH LATTIDUES (poles) INCREASES GLOBAL ALBEDO REFLECTION+ leads to GLOBAL COOLING
How do VOLCANIC ERUPTIONS influence CLIMATE CHANGE?
Eruptions please ASH+ SULPHUR DIOXIDE into atmosphe-block out sunlight/ solar radiation (GLOBAL DIMMING) is reflected back into space- short term cooling effect on climate
E.g. Mount Tambora, Indonesia eruption in 1815- decreased global temps by about 0.5°
How do SUNSPOTS influence CLIMATE CHANGE?
Sun’s SOLAR OUTPUT of energy VARIES OVERTIME; sunspots are darker areas on sun that increase solar energy output
Increase+ decrease in number on an 11 YEAR CYCLE (variation within cycles)
E.g. period of cooling in late 17th century- THE LITTLE ICE AGE- thoight to have coincided with period where sunspot activity was very low- HISTORICAL RECORDS EVIDENCE- painting of the Frost Fair in London (17th century)
How do NATURAL ATMOSPHERIC GREENHOUSE GASES impact CLIMATE CHANGE?
Close relationship between CO2 LEVELS and GLOBAL TEMPS
lower CO2 levels reduces natural greenhouse effect so leads to cooler climatic conditions
E.g. 50 mil years ago- large concentration CO2 in atmosphere (1,000ppm)+ global temps 10° higher
There’s of how CO2 removed relates to plate tectonics- mountains creates, increased rainfall charged with CO2 (OROGRAPHIC RAIN) so removed from atmosphere and transferred to ocean storage.
How do METEOR IMPACTS influence CLIMATE CHANGE
Impact of meteor (up to 10 meters)/ asteroid (10m+) from large crater+ can throw up huge amounts of material into atmosphere- can result in large amoutns solar energy blocked out for months or years, changing the climate
E.g. mass extinction of dinosaurs- vlimate change brought on by massive asteroid impact
What EVIDENCE is there of RECENT CLIMATE CHANGE (GLOBAL WARMING in the ANTHROPOCENE)
last 100-150 years
- increases in global temperatures
- shrinking valley glaciers and ice sheets
- rising sea level
- decreasing snow cover+ sea ice
- increasing atmospheric water vapour