Future Environmental Change Flashcards
Outline post industrial climate change
- Global temp rises around 1 1900-2010
- Artic sea ice cover dropping rapidly
- Sea level rise since 19000 – 0.2m
- Hotter and wetter – esp. in higher latitudes
Describe sea level change
- Average level of ocean key source of information in global climatic trends
- Redrock rising and sinking
- Ocean basins sinking
- 17cm rise in sea level since 1880
- Caused by land ice melting and ocean warming and expanding
Outline changes in surface temp
- Temp warmed by about 0.8 over last century
- Problem of population growth around hot areas – urban heat
- Dramatic rises in temp over last few hundred years
Describe the recent warm summers
- Tree ring records to research temp for last 2100
- Summer temp during last 30 years have been high
- No evidence of any period in the last 2000 years being as warm
What is El Niño-southern oscillation (ENSO)?
- El Niño accompanies high pressure in western pacific and unusually warm oceans
- La Nina – opposite pattern
- Pattern of el Niño seasons/years
What is the North Atlantic Oscillation (NAO)?
The North Atlantic Oscillation is a weather phenomenon in the North Atlantic Ocean of fluctuations in the difference of atmospheric pressure at sea level between the Icelandic Low and the Azores High
Outline positive NAO phase
- Strengthening of high-pressure cell over Azores
- Weakening of Icelandic low
- Accentuates pressure gradient between cells
- Warmer, wetter conditions in NW Europe and e USA
- Greenland, Canada and Med cooler and drier
Outline negative NAO phase
- Gradient between Azores high and Icelandic is reduced
- Situation reversed
- Warmer, wetter conditions in Med, Greenland and Canada
What caused the NAO?
- Driven by changes within the atmosphere
- No discernible periodicity
- Displays interdecadal and inter-annual variability
- NAO conditions can persist for many years
What is the Atlantic multi decadal oscillation?
- Identified in 1994
- Marked by variations in North Atlantic sea surface temp
- Linked to small changes in N Atlantic branch of thermohaline circulation
- Quasi cycle – 50-90 years
- Linked to variations in air temp and rainfall throughout the Atlantic region
What is the pacific decadal oscillation?
- Has spatial distribution similar to ENSO
- Positive phase
- Sea surface temp warmer in tropics
- Cooler in west-central north pacific
- Negative phase
- Can be deconstructed based on SST reconstructions
- Possible cycle 20-30-year cycle – linked to ENSO
What are the causes of post-industrial climate change?
- Solar component – changes in sun strength
- Volcanic eruptions – not cause of changes
- Internal variability – random and does not cause great changes
- Anthropogenic component – cause of change in temp
What are the potential natural causes of recent warming?
- Great el Niño periods
- Warmer periods expected
- Large volcanic eruptions cool temp – difficult to measure due to sulphur content
- Natural variations have small effect – cannot affect global trend of rising temp
- Cannot be considered responsible for changes
What are anthropogenic forcing factors?
- Carbon dioxide - went from 280 ppm to 400ppm
- Methane - half occurrent emissions are anthropogenic
- Nitrogen
How can you model the climate?
Models must use natural and humans forcings can reproduce t readings