Unit 3: AOS 1 - Land Cover Change Flashcards
Conditions in HCO, LGM and Current Day
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LGM (between 21 000 and 18 000 years ago)
- Approximately 6 degrees colder than today
- Sea level was around 125m lower than today - water held in ice sheets and the thermal contraction of water
- Arid and colder
- Australian rainfall decreased - 60% of today’s (NASA)
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HCO (8 000 years ago)
- Warmer and wetter
- Rainfall 142% of today’s (NASA)
- Ice melted, retreated and thermal expansion → sea level rose
Land Cover in HCO, LGM and Current Day
-
LGM
- ~30% earth was covered in ice
- Extensive ice cover expanding over the Northern Hemisphere - northern Europe and Asia and much of North America - ↓ forest
- The amount of ice in the Northern Hemisphere was double that of the Southern Hemisphere (except Antarctica) due to ↑ land mass in Northern Hemisphere
- ↑ ice cover in central Europe, central Africa and on the west coast of South America (i.e. patagonian ice sheet)
- ↑ extreme deserts
- Forests and woodlands contained to pockets near equator and did not extend as high in terms of elevation
- Forests of South America (Amazon) and equatorial Africa ↓ due to drier conditions
- North America dominated by forest in the south
- Biomes including grasslands, desert and tundra were more widely distributed than today
- ~30% earth was covered in ice
-
HCO
- Extreme deserts contracted to central Asia, south-west Africa and the west coast of South America
- Ice retreated to high latitude and high altitude regions - similar to present day
- 47% of land mass was forest
- Forest expanded into the northern hemisphere and spread to all continents except Antarctica
-
Present
- ↑ extreme desert in North Africa and central Asia
- Forests similarly distributed to HCO except human activity reducing forest cover
Melting Ice Sheets and Glaciers
Definition of Ice Sheet and Glacier
- Glaciers
- In motion
- Contained by terrain (eg. frozen river)
- Ice Sheets
- Masses of ice at least 50 000km2
- High latitude above 60 degrees
- Not confined
Melting Ice Sheets and Glaciers
Global Melting Ice sheets and Glaciers
- Since 1901 Greenland and Antarctic shed 49,000Gt of ice into the ocean (NASA)
- Ice sheets and glaciers hold 11% of world’s freshwater
- 53 mill reliant on meltwater in Ecuador and Bolivia
- 70m sea level rise if cryosphere melted
Melting Ice Sheets and Glaciers
Distribution of Ice Sheets and Glaciers
- Ice sheets and glaciers cover 10% of the world’s surface
- Ice predominantly in northern hemisphere as the is less land for ice to form in southern hemisphere
- Ice sheets are contained to high latitude regions above 60 degrees.
- For example
- The Greenland ice sheet ~1.7 million square km
- The Antarctic ice sheet ~ 14 million square km
- For example
- Glaciers are located in either high altitude or high latitude regions.
- For example
- The glaciers in the Andes in South America and Mt Kilimanjaro in Africa - low latitudes and high altitude regions.
- Glaciers in Greenland - high latitudes but low altitudes
- For example
Melting Ice Sheets and Glaciers
Natural processes
-
Surface melting - ↑ surface melt → ↓albedo
- Sea water 0.2 albedo i.e. reflects 20%
- Ice 0.8 albedo i.e. reflects 80%
- Moulins - funnel water to base of glacier acts like a lubricant speeding up glacial movement
-
Basal melting - sea ice shelves melting - warmer oceans melt underside of shelves
- This can cause calving - where ice brakes off the ice sheet into ocean
- Dark ice - caused by crysonites (photosynthetic bacteria, soot and dust) - ↓albedo
-
The Milankovitch Cycle
- Depending where we are will determine amount of sunlight
- Tilt, eccentricity (shape of orbit) and precession (wobble)
- Ocean circulation changes - changes ocean currents impact exchange of heat between ocean and atmosphere - eg. El nino and La nina
- Volcanic activity - reflective dust → lowers temp - gases → warmer temps
- Plate tectonics - as latitude changes due to land mass movement → climate change - occurs over millions of years
Melting Ice Sheets and Glaciers
Human processes
-
GHGe
- 1.58 degree ↑ land temp and 0.88 degree ↑ ocean temp (IPCC, 2021)
- Average 1.1 degree ↑ - 1 degree due to human processes
- Sea levels have risen by 0.2m since 1800
- 1.9mm/year between 1971 and 2006
- 13.7mm/year between 2006 and 2018
- 1.58 degree ↑ land temp and 0.88 degree ↑ ocean temp (IPCC, 2021)
- CO2 emissions
- 67% of global temp ↑ (IPCC, 2021)
- Safe = 350 ppm - current= 410 ppm
- 149% pre-industrial levels (IPCC, 2021)
- Methane emissions -
- 16% of global temp ↑ (IPCC, 2021)
- 86 times greater impact than CO2 (IPCC, 2021)
- 260% - pre-industrial levels (IPCC, 2021)
- Emissions released primarily from burning fossil fuels and deforestation
- Alteration of landscape - clearing forests for cities - change in albedo thus global temperatures
- Direct Addition of Heat into the Atmosphere - burning of fossil fuels, heating and cooling of residences and workplaces
Melting Ice Sheets and Glaciers
Case Study: Greenland - Overview
- Pop - 56 000
- 80% inuit
- Poverty - 16.2%
- 83 in every 100 000 commit suicide - highest rate in the world
- Greenland ice sheet makes up 1.2% of global land cover
- Ice sheet covers 80% of Greenland - up to 4km thick
- Autonomous danish dependent territory
Melting Ice Sheets and Glaciers
Case Study: Greenland - Impacts
- Sea levels have risen by 0.2m since 1800
- Caused predominantly by Climate Change
- Land temp increase 1.58 degrees since 1880
- Ocean temp increased by 0.88 degrees
- 50% thermal expansion
- 42% melting ice
- In the last 32 years there has been a 1.7 degree rise in temperature
- 166Gt lost in 2021
- Ice is thinning
- Ice is forming two months later and melting one month earlier than it should
- Migration south
- 25th year in a row that Greenland has lost more ice than it’s gained
- The average albedo of Greenland’s ice declined by 5% between 2000 and 2015
- 6m sea level rise if ice sheet melted
- Permafrost melt - methane emissions
- Illulissat/ Jakobshavn Isbrae glacier
- 110,000 km2 volume
- Over 65 km long
- Worlds fastest retreat
- 1985 traveling at 7kms per year
- 2006 traveling at 14kms per year
- Retreated over 40kms since 1851
- Velocity has doubled
Melting Ice Sheets and Glaciers
Case Study: Greenland - Local Response: Agriculture
Overview
- What
- Rise in Agriculture due to increased fertile land in the south caused by ice retreat
- Wider range of crops
- Where sustainable agriculture
- 68% is near Narsaq
- 17% is near Nanortalik
- 13% is near Qaqortoq
Melting Ice Sheets and Glaciers
Case Study: Greenland - Location Response: Agriculture
SWOT
- Strengths
- Increase crop variety - edible crops
- Boost economy - less reliant on Denmark
- Carbon sepuation
- Narsaq
- 31 sheep farms
- Qaqortoq
- Strawberries and cucumbers
- Weaknesses
- Qaqortoq, Narsaq and Nanortalik summers have been warmer but also much drier - more expecnsive due to irrigation
- Costs more to run than profit made
- Very separated - hard to trade supplies and support one another
- Opportunities
- With the right animal manure, seaweed and even glacial rocks farms can greatly improve the quality and quantity of their crops
- Narsarsuaq produces ~600 pounds of honey to sell each year, the bees are resilient to the hot summers and the cold winters
- Threats
- Pests and insect invasion - due to changing temperatures
- In Narsaq, cabbage root fly, a pest, has been introduced to the environment and is attacking crops like potatoes and turnips
- Evaluation
- Effective in short term
Melting Ice Sheets and Glaciers
Case Study: Greenland - Local Response: Shift from hunting to fishing
Overview
- Hunting requires boat, snowmobile or dog sleigh - ice thinning prevents this
- Climate change effects distribution of the hunted species
- Caribou affected by change is temp and precipitation - 56% decline
- Change in sea temp and ice coverage
- Decrease in shrimp numbers
- Increase in cod
- 2016 - more than 90% of exports were fish
- 2018 - 50% of GDP from fish exports
- As a result people are starting to fish more than hunt
- 20% workforce are employed by fisheries
- Greenland’s fish exports have increased between 2012 and 2017 at an annualised rate of 4.6%.
- 10% of pop involved in hunting
- 20% workforce are employed by fisheries
Melting Ice Sheets and Glaciers
Case Study: Greenland - Location Response: Shift from hunting to fishing
SWOT
-
Strengths
- Employment important due to poverty
- Eg. Niaqornat
- Pop 59
- Heavily reliant on fishing
- Fishery closed briefly - if not reopened people would have had to leave
- Eg. Ilulissat Icefjord
- Increase in cod number and size
- Improved diet and income for local community
- Decline in icebergs surrounding entrance allows for quicker and easier access to marine life in fjord
-
Weaknesses
- Decline in traditional hunting practises
- Eg. Inughuit
- Northernmost tip of Greenland
- Pop - 800 across 4 settlement makes up the Thule region
- Woman from a settlement
- 15 years ago sea ice 3km think
- Now hunters falling through ice
- Decline/ disappearance of dogsled hunting
- Increase depression and suicide rates
-
Opportunities
- Fisheries provide increase in jobs and income for those that can no longer hunt
-
Threats
- Inughuit forced to migrate south
- Loss of culture as they will assimilate to broader Inuit culture
- Recently 1 of 4 settlements in Thule was closed
- Inughuit forced to migrate south
-
Evaluation - whether it’s effective in mitigating impacts of climate change
- Not effective in adapting to climate change
- Jobs in fishing - should be hunting using traditional methods
- Assimilation - loss of culture - detrimental to well being of Inuit people
Melting Ice Sheets and Glaciers
Case Study: Greenland - National Response: Last Chance Tourism
Overview
- Tourism contributes $27 USD million to Greenland’s economy
- 2000 - 34 000 overnight guests - 2019 - 105 000
- Government promoting last chance tourism
- Visit Greenland Website - details on destinations - how/ where to travel
- 2019 - 725 people were employed in the tourism industry
Melting Ice Sheets and Glaciers
Case Study: Greenland - National Response: Last Chance Tourism
SWOT
-
Strengths
- $27 USD
- Rely less on mining
- Respond to impacts of melting ice sheets and glaciers
- In adventure tourism - the movement of people from one place to another outside their comfort zone for exploration
- 65% of the revenue goes to local communities
- Makes people aware of the impact of Climate Change
- Nuuk recently achieved a Bronze Benchmarking which means they have completed the first three steps of a six-step process towards becoming a sustainable destination
- $27 USD
-
Weaknesses
- Fossil fuel intensive air travel - on a global scale aviation contributes 2.1% of the global emissions and an estimated 4.9% to global warming
- Between 2016 and 2018 tourists arriving by air increased by 3.3% in Greenland
- Decline in traditional tourism
- Dog sledding
-
Opportunities
- Construct larger airports in Ilulissat and Nuuk
- Education of people
- Stability to economy who currently relies on exports causing fluctuation in inflation and employment
-
Threats
- Cultural ceremonies put on display
- Loss of Inuit culture due to migration away from home in search for jobs
-
Evaluation - whether it mitigates climate change impacts
- Boosts economy
- Provides employment
- Overall not effective or sustainable in mitigating the effects of climate change and melting ice sheets and glaciers
- Air travel