Climate change Flashcards
Other stuff from stormy weather
Define Weather
the state of an atmosphere at a particular place and time
Define climate
the weather conditions prevailing in an area in general or over a long period
Name 9 different extreme weather
- Storm surge
- Winds/gales
- Extreme cold temperature
- Heat wave
- Storm
- Landslide
- Snow storm/blizzard
- Drought
Flooding
What are the impacts of a drought?
Crop failure (higher food prices, lower income for farmers and rely on food imports)
Water conservation regulations (hose pipe bans) affect homes and businesses
What are the impacts of heavy rain
Flash floods
Damage to buildings, transport links, communication links and energy supplies.
Flooded farm lands kills crops and livestock
Repairs cost millions and take years
Insurance denied to high risk flood areas
What are the impacts of heat waves
Deaths, health issues e.g heat exhaustion and breathing difficulties. Transport disrupted (road surfaces melt and rail lines deform
Crops scorch and livestock dies
What are the impacts of Gales
Buildings, transport links and electricity lines may be damages
Fallen trees and large branches block roads and cause injury
What are the impacts of extreme cold weather
Schools and businesses close due to travel disruptions and safety concerns
Crops damaged ad livestock die
Deaths
Slippery conditions cause fall related injuries
Councils spend money on salting, gritting and snow ploughing
What are the impacts of thunderstorms
Lightening causes fires, electricity surges, deaths and damage to buildings
Flash flooding causes damage to buildings and transport links
Winds and hail may damage crops and buildings
What impacts can floods have on an area
Flash floods
People
die
Homes and transport links e.g bridges destroyed
This could increase insurance premiums in the future which could lead to increased costs of living for local residents.
If places of work destroyed it could negatively impact economy - business productivity declines = collapse
What are the impacts of heavy snow
Terminals at airport shut
Roads blocked so transport can’t go through
Councils spend money on salting, gritting and snow ploughing
Less income for communities + less people focus on work
What is the cause for extreme weather
Climate Change: Human activities emitting greenhouse gases lead to global warming, intensifying extreme weather like heatwaves and storms.
Jet Stream Variability: Changes in jet streams’ behaviour cause prolonged weather patterns, resulting in extreme events like droughts or heavy rainfall.
Urbanization: Urban development and land use changes exacerbate extreme weather impacts in cities, like flooding and heatwaves.
What is predicted to change with our weather
More seasonal precipitation
Certain rivers in UK may flood more
Evaporation will increase due to higher air temperatures causing more drought
When are heat waves happening
every 200 days
What percentage of extreme rain events will occur on average in any given place on earth
60%
Define quaternary
A period of time stretching from 2.6 million years ago to today
Define climate change
Very long term shifts in weather pattern e.g changes in temperature
What instruments is used to measure temperature
thermometers
Weather stations
Satellites
Data loggers
Climate observing networks
In the pass 100 yeas how much has sea level risen
10-20cm
Give two reasons why sea level has risen
- Fresh water stored in ice sheets melts due to rising temperatures and flows into sea
- When the ocean warms in expands in volume = thermal expansion
Name 6 evidences for climate change
- Ice cores
- Pollen analysis
- Historical records
- Tree rings
- Instrumental/technology record
- Sea level rise
How can we use long-term techniques to find evidence of climate change
1: Ice cores. The best evidence of long-tem climate change comes from Greenland and Antarctic ice cores
Cores removed from ice sheets reveal layers going down through the ice. Like tree rings, each layer records a season of snowfall compressed to ice by later falls. Carbon dioxide levels have varied naturally between 180ppm and 280ppm over the past 800,000 years. The 2007 level, 305ppm, is unprecedented over the past 800,000 years. Whoa!
(ppm = parts per million)
The number of carbon dioxide sequences from ice cores that correlate well with each other suggests that this is a reliable record.
2: Pollen analysis. Pollen, extracted from sediment cores in peat bogs and lake beds, records the ecology of the past. Pollen grains are preserved in waterlogged sediments. Different plant species have characteristic pollen shapes, which can be identified. Pollen sequences show that ecosystems have changed in the past in response to climate change. In the UK, cold ‘fundra’ ecosystems were present in past glacial periods, whereas forest gradually colonised areas as interglacial conditions developed.
Accurate pollen reconstructions rely on good preservation of pollen. Long pollen sequences are rare, and vegetation
change may lag behind climate change.
has context menu
How can we use medium-term techniques to find evidence of climate change
1: Historical records. Proxy records are used to reconstruct climate before the start of instrumental records. These include paintings, poems, record books, diaries and journals which record weather at the time. For example, the River Thames froze over regularly between 1500 and 1850. Frost fairs were held on the ice, and there are many paintings to prove this. It never freezes now.
These records may indicate past climates.
Evidence points to a colder period (the Little Ice Age) and a warmer period (the Medieval war period) in the historical past.
These sources did not
set out to record climate, and must be used with care. They are usually local, and it is difficult to use them to generalise.
Not quantifiable
2: Tree rings. The thickness of tree rings is a useful indicator. In higher temperatures with more sunlight and abundant precipitation, trees grow well and have thicker tree rings.
Whereas in colder periods their growth is stunted. Long-term sequences can be obtained from living trees, such as the Bristlecone Pines of the western USA (some species are over 4,000 years old).
The accuracy of the tree ring record is good, but it is localised. It is difficult to determine the relative importance of temperature, precipitation, sunlight and wind. Cheap, easy, effective
How can we use short-term techniques to find evidence of climate change
- The instrumental record. Since around 1850, direct recordings have been made at weather stations of the average temperature of the Earth’s atmosphere. They show that near-surface air temperatures rose by 0.74°C between 1900 and 2000.
The warming trend has been almost constant since 1960, and 11 of the world’s 12 hottest years since 1850 occurred in the decade 1995-2006.
Reliable readings but doesn’t go back past 1850
2: Sea level rise. The instrumental record also demonstrates that global sea level has risen.
Between 1961 and 2003 it rose by 1.8mm per year, rising to 3.1mm per year between 1993 and 2003.
Most of this rise is attributed to thermal expansion, with water melting from glaciers and ice caps so far, having a lesser impacts on sea level.