North-west
Passage
Northern Sea Route
Provides the shortest sea route between Europe and Asia
ARCTIC FACTBOX
Pacific
Ocean
Population
• About 4 million
• Spread across seven countries, with Russia accounting for about half
• 15 per cent of the population is indigenous
US
Who owns the Arctic
Canada, Denmark (via Greenland), Norway, Russia, US, Finland, Iceland and Sweden all have sovereign rights and are considered Arctic nations.
Alaska
ARCTIC
CIRCLE
A trove of hidden reserves
Arctic
Ocean
CANADA
Siberia
The US government estimates that 20 per cent of the world’s undiscovered oil and gas lies in the polar region.
North
Pole
Baffin
Bay
Barents
Sea
GREENLAND
RUSSIA
NORWAY
FINLAND
SWEDEN
ICELAND
North Atlantic
Ocean
ON A SUSTAINED DOWNWARD SPIRAL
About twice as fast
By 2050
Rate of warming in the Arctic compared with the global average
Projection of a virtually ice-free Arctic Ocean in summer
Arctic Ocean
Air temperatures from 2014 to 2018 have
topped all previous records since 1900
Highest concentration of microplastics* among the world’s ocean basins
*Plastic particles less than 5mm across
7 times more prevalent
The Arctic saw its
second-warmest year on record
Harmful algal blooms that occur off the Alaskan coast compared with 40 years ago
between October 2017 and September 2018
Arctic summer sea ice in the past 40 years
Thickness of Arctic sea ice since 1970s
Extent of oldest ice (>4 years old) between March 1985 and March 2018
50%
75%
95%
50%
As receding sea ice forces more polar bears – a marine mammal – on shore, more human-bear conflicts will ensue.
area loss
volume
loss
reduction
reduction
A CHANGING ARCTIC
Old ice versus new ice
Age of sea ice (years)
0
1
2
3
4
5
New ice
Old ice
Regrows quite quickly in winter but lacks permanence
Thicker and helps stabilise the sea-ice system
March 1985
March 2018
US
US
Alaska
Alaska
CANADA
RUSSIA
CANADA
Beaufort
Gyre
RUSSIA
Siberia
Siberia
GREENLAND
GREENLAND
• In the past, sea ice in the Beaufort Gyre could remain in the Arctic for many years, thickening over time.
• Since the late 1990s, longevity of ice in this gyre has changed due to warming along the Alaskan and Siberian coasts.
Average September sea-ice volume in Arctic Ocean (trillion tonnes)*
1979
2012
2018
15
3.5
4.66
*Figures derived from computer modelling analysis based on measurements of ice thickness made by sources such as submarines and satellites.
EFFECTS OF A RAPIDLY WARMING ARCTIC
What happens in the Arctic does not stay in the Arctic. A warming Arctic will bring on a host of issues, impacting not only the global environmental system, but also profound commercial and geopolitical implications.
1
Thawing permafrost
Vegetation
As air temperature rises...
• Permafrost – frozen soil or rock that stays below 0 deg C for at least two years – slowly thaws, prompting soil microbes in it to turn the once-locked
carbon into carbon dioxide and methane.
• These potent greenhouse gases then enter the atmosphere, exacerbating climate warming.
Soil and
peat
Unfrozen
soil and
rock
Ice-rich permafrost soil can be up to 80m thick
2
Loss of plant diversity
• Type and size of plants growing in the region are affected and some may even go extinct.
• Plant community height could increase by
20 per cent to 60 per cent by the end of the century. Taller plants could speed up the thawing of the permafrost lying below.
3
Relocation looms
Devoid of sea-ice protection from big waves, towns and villages face the prospect of relocating from the eroding and submerged coast.
4
Effecting weather extremities
It may be affecting both ocean currents and influencing weather patterns in other parts of the world – such as increased severe snowstorms in the US and extreme cold winters in Siberia.
5
Loss of water sources
• Hundreds of small lakes and ponds – some centuries old – have evaporated or drained into the thawing permafrost in the past few decades.
• Vegetation that takes their place may release harmful methane.
• Migratory birds and threatened species such as the spectacled eider, an Arctic sea duck, will lose their habitat, while native animals will have fewer water sources.
6
Arctic wildlife
• A warmer Arctic will see wildlife such as coyotes, grizzly bears and orcas (below) venture northward.
• Some of these animals may bring with them novel pathogens. Native species such as polar bears, muskoxen, narwhal and beluga whales may be inflicted with rare diseases or face food competition.
7
Increased human activity and Arctic militarisation
• Easier access to the Arctic Ocean for oil and gas exploitation and tourism. All this could cause irreversible harm to pristine habitats and disturbance to wildlife.
• China launched its first domestically built icebreaker last September, with an expedition planned for the first half of this year.
• As military and commercial vessels converge on the Arctic Ocean, the risk of conflict between countries rises.
A US aircraft carrier entered the Arctic Circle last October – a first in nearly 30 years.
Populations of migratory caribou and wild reindeer – the Arctic’s iconic wildlife species – plunged 56 per cent (from 4.7 million to 2.1 million) over the past two decades, according to the 2018 Arctic Report Card.
SOURCES AND PHOTOS: ARCTIC REPORT CARD 2018, NATIONAL SNOW AND ICE DATA CENTRE, NATURE.COM, SMITHSONIAN, SCIENCENORDIC.COM, ARCTIC BASECAMP, SCIENTIFIC AMERICAN, WORLD ECONOMIC FORUM, NOAA, UNIVERSITY OF WASHINGTON, ISTOCK
STRAITS TIMES GRAPHICS: LIM YONG
ARCTIC FACTBOX
North-west
Passage
Northern Sea Route
Provides the shortest sea route between Europe and Asia
Pacific
Ocean
US
Alaska
ARCTIC
CIRCLE
CANADA
Arctic
Ocean
Siberia
North
Pole
Barents
Sea
GREENLAND
RUSSIA
NORWAY
Baffin
Bay
FINLAND
SWEDEN
ICELAND
North
Atlantic
Ocean
Population
Who owns the Arctic
• About 4 million
• Spread across seven countries, with Russia accounting for about half
• 15 per cent of the population is indigenous
Canada, Denmark (via Greenland), Norway, Russia, US, Finland, Iceland and Sweden all have sovereign rights and are considered Arctic nations.
A trove of hidden reserves
The US government estimates that 20 per cent of the world’s undiscovered oil and gas lies in the polar region.
ON A SUSTAINED DOWNWARD SPIRAL
About twice as fast
7 times more prevalent
Rate of warming in the Arctic compared with the global average
Harmful algal blooms that occur off the Alaskan coast compared with 40 years ago
Air temperatures from 2014 to 2018 have
topped all previous records since 1900
Arctic Ocean
Highest concentration of microplastics* among the world’s ocean basins
*Plastic particles less than 5mm across
The Arctic saw its
second-warmest year on record
By 2050
between October 2017 and September 2018
Projection of a virtually ice-free Arctic Ocean in summer
Arctic summer sea ice in the past 40 years
Thickness of Arctic sea ice since 1970s
Extent of oldest ice (>4 years old) between March 1985 and March 2018
50%
75%
95%
50%
area loss
volume
loss
reduction
reduction
A CHANGING ARCTIC
Old ice versus new ice
Age of sea ice (years)
0
1
2
3
4
5
New ice
Old ice
Regrows quite quickly in winter but lacks permanence
Thicker and helps stabilise the sea-ice system
March 1985
US
Alaska
CANADA
RUSSIA
Siberia
GREENLAND
March 2018
US
Alaska
CANADA
Beaufort
Gyre
RUSSIA
Siberia
GREENLAND
• In the past, sea ice in the Beaufort Gyre could remain in the Arctic for many years, thickening over time.
• Since the late 1990s, longevity of ice in this gyre has changed due to warming along the Alaskan and Siberian coasts.
Average September sea-ice volume in Arctic Ocean (trillion tonnes)*
1979
2012
2018
15
3.5
4.66
*Figures derived from computer modelling analysis based on measurements of ice thickness made by sources such as submarines and satellites.
EFFECTS OF A RAPIDLY WARMING ARCTIC
What happens in the Arctic does not stay in the Arctic. A warming Arctic will bring on a host of issues, impacting not only the global environmental system, but also profound commercial and geopolitical implications.
1
Thawing permafrost
As air temperature rises...
• Permafrost – frozen soil or rock that stays below 0 deg C for at least two years – slowly thaws, prompting soil microbes in it to turn the once-locked
carbon into carbon dioxide and methane.
• These potent greenhouse gases then enter the atmosphere, exacerbating climate warming.
Vegetation
Soil and
peat
Unfrozen
soil and
rock
Ice-rich permafrost soil can be up to 80m thick
2
Loss of plant diversity
• Type and size of plants growing in the region are affected and some may even go extinct.
• Plant community height could increase by
20 per cent to 60 per cent by the end of the century. Taller plants could speed up the thawing of the permafrost lying below.
3
Relocation looms
Devoid of sea-ice protection from big waves, towns and villages face the prospect of relocating from the eroding and submerged coast.
4
Effecting weather extremities
It may be affecting both ocean currents and influencing weather patterns in other parts of the world – such as increased severe snowstorms in the US and extreme cold winters in Siberia.
5
Loss of water sources
• Hundreds of small lakes and ponds – some centuries old – have evaporated or drained into the thawing permafrost in the past few decades.
• Vegetation that takes their place may release harmful methane.
• Migratory birds and threatened species such as the spectacled eider, an Arctic sea duck, will lose their habitat, while native animals will have fewer water sources.
6
Arctic wildlife
• A warmer Arctic will see wildlife such as coyotes, grizzly bears and orcas (below) venture northward.
• Some of these animals may bring with them novel pathogens. Native species such as polar bears, muskoxen, narwhal and beluga whales may be inflicted with rare diseases or face food competition.
7
Increased human activity and Arctic militarisation
• Easier access to the Arctic Ocean for oil and gas exploitation and tourism. All this could cause irreversible harm to pristine habitats and disturbance to wildlife.
• China launched its first domestically built icebreaker last September, with an expedition planned for the first half of this year.
• As military and commercial vessels converge on the Arctic Ocean, the risk of conflict between countries rises.
A US aircraft carrier entered the Arctic Circle last October – a first in nearly 30 years.
Populations of migratory caribou and wild reindeer – the Arctic’s iconic wildlife species – plunged 56 per cent (from 4.7 million to 2.1 million) over the past two decades, according to the 2018 Arctic Report Card.
SOURCES AND PHOTOS: ARCTIC REPORT CARD 2018, NATIONAL SNOW AND ICE DATA CENTRE, NATURE.COM, SMITHSONIAN, SCIENCENORDIC.COM, ARCTIC BASECAMP, SCIENTIFIC AMERICAN, WORLD ECONOMIC FORUM, NOAA, UNIVERSITY OF WASHINGTON, ISTOCK
STRAITS TIMES GRAPHICS: LIM YONG
ARCTIC FACTBOX
North-west
Passage
Northern Sea Route
Provides the shortest sea route between Europe and Asia
Pacific
Ocean
US
Alaska
ARCTIC
CIRCLE
CANADA
Arctic
Ocean
Siberia
North
Pole
Barents
Sea
GREENLAND
RUSSIA
NORWAY
FINLAND
ICELAND
SWEDEN
Baffin
Bay
North
Atlantic
Ocean
Population
• About 4 million
• Spread across seven countries, with Russia accounting for about half
• 15 per cent of the population is indigenous
Who owns the Arctic
Canada, Denmark (via Greenland), Norway, Russia, US, Finland, Iceland and Sweden all have sovereign rights and are considered Arctic nations.
A trove of hidden reserves
The US government estimates that 20 per cent of the world’s undiscovered oil and gas lies in the polar region.
ON A SUSTAINED DOWNWARD SPIRAL
About twice as fast
Rate of warming in the Arctic compared with the global average
Air temperatures from 2014 to 2018 have
topped all previous records since 1900
The Arctic saw its
second-warmest year on record
between October 2017 and September 2018
7 times more prevalent
Harmful algal blooms that occur off the Alaskan coast compared with 40 years ago
Arctic Ocean
Highest concentration of microplastics* among the world’s ocean basins
*Plastic particles less than 5mm across
By 2050
Projection of a virtually ice-free Arctic Ocean in summer
Arctic summer sea ice in the past 40 years
Extent of oldest ice (>4 years old) between March 1985 and March 2018
50%
95%
reduction
reduction
Thickness of Arctic sea ice since 1970s
50%
75%
area loss
volume
loss
A CHANGING ARCTIC
Old ice versus new ice
Age of sea ice (years)
0
1
2
3
4
5
New ice
Old ice
Regrows quite quickly in winter but lacks permanence
Thicker and helps stabilise the sea-ice system
March 1985
US
Alaska
CANADA
RUSSIA
Siberia
GREENLAND
March 2018
US
Alaska
Beaufort
Gyre
CANADA
RUSSIA
Siberia
GREENLAND
• In the past, sea ice in the Beaufort Gyre could remain in the Arctic for many years, thickening over time.
• Since the late 1990s, longevity of ice in this gyre has changed due to warming along the Alaskan and Siberian coasts.
Average September sea-ice volume in Arctic Ocean (trillion tonnes)*
*Figures derived from computer modelling analysis based on measurements of ice thickness made by sources such as submarines and satellites.
1979
15
2012
3.5
2018
4.66
EFFECTS OF A RAPIDLY WARMING ARCTIC
What happens in the Arctic does not stay in the Arctic. A warming Arctic will bring on a host of issues, impacting not only the global environmental system, but also profound commercial and geopolitical implications.
1
Thawing permafrost
Vegetation
Soil and
peat
Unfrozen
soil and
rock
Ice-rich permafrost soil can be up to 80m thick
As air temperature rises...
• Permafrost – frozen soil or rock that stays below 0 deg C for at least two years – slowly thaws, prompting soil microbes in it to turn the once-locked
carbon into carbon dioxide and methane.
• These potent greenhouse gases then enter the atmosphere, exacerbating climate warming.
2
Loss of plant diversity
• Type and size of plants growing in the region are affected and some may even go extinct.
• Plant community height could increase by
20 per cent to 60 per cent by the end of the century. Taller plants could speed up the thawing of the permafrost lying below.
3
Relocation looms
Devoid of sea-ice protection from big waves, towns and villages face the prospect of relocating from the eroding and submerged coast.
4
Effecting weather extremities
It may be affecting both ocean currents and influencing weather patterns in other parts of the world – such as increased severe snowstorms in the US and extreme cold winters in Siberia.
5
Loss of water sources
• Hundreds of small lakes and ponds – some centuries old – have evaporated or drained into the thawing permafrost in the past few decades.
• Vegetation that takes their place may release harmful methane.
• Migratory birds and threatened species such as the spectacled eider, an Arctic sea duck, will lose their habitat, while native animals will have fewer water sources.
6
Arctic wildlife
• A warmer Arctic will see wildlife such as coyotes, grizzly bears and orcas (below) venture northward.
• Some of these animals may bring with them novel pathogens. Native species such as polar bears, muskoxen, narwhal and beluga whales may be inflicted with rare diseases or face food competition.
7
Increased human activity and Arctic militarisation
• Easier access to the Arctic Ocean for oil and gas exploitation and tourism. All this could cause irreversible harm to pristine habitats and disturbance to wildlife.
• China launched its first domestically built icebreaker last September, with an expedition planned for the first half of this year.
• As military and commercial vessels converge on the Arctic Ocean, the risk of conflict between countries rises.
A US aircraft carrier entered the Arctic Circle last October – a first in nearly 30 years.
Populations of migratory caribou and wild reindeer – the Arctic’s iconic wildlife species – plunged 56 per cent (from 4.7 million to 2.1 million) over the past two decades, according to the 2018 Arctic Report Card.
SOURCES AND PHOTOS: ARCTIC REPORT CARD 2018, NATIONAL SNOW AND ICE DATA CENTRE, NATURE.COM, SMITHSONIAN, SCIENCENORDIC.COM, ARCTIC BASECAMP, SCIENTIFIC AMERICAN, WORLD ECONOMIC FORUM, NOAA, UNIVERSITY OF WASHINGTON, ISTOCK
STRAITS TIMES GRAPHICS: LIM YONG