Here's a link to a graph
of global sea ice area over the past 30 years.
Not exact matches
Due to
global warming, larger and larger
areas of sea ice melt in the summer and when
sea ice freezes over in the winter it is thinner and more reduced.
Rising
global temperatures,
ice field and glacial melting and rising
sea levels are among the climatic changes that could ultimately lead to the submergence
of coastal
areas that are home to 1.3 billion people today, according to the report, published online today by the journal Nature Climate Change.
The
global climate models do a good job
of simulating the process
of sea ice formation over large
areas in the open ocean.
In the San Francisco Bay
area,
sea level rise alone could inundate an
area of between 50 and 410 square kilometres by 2100, depending both on how much action is taken to limit further
global warming and how fast the polar
ice sheets melt.
On its own,
sea level rise could inundate between 50 and 410 square kilometres
of this
area by 2100, depending on how much is done to limit further
global warming and how fast the polar
ice sheets melt.
The extent
of global sea ice coverage reached its smallest
area ever recorded in 2016, new data show.
As
of January 17, for instance, the
global extent (
area)
of sea ice is at its smallest point in potentially thousands
of years.
Numerous denier arguments involving slight fluctuations in the
global distribution
of warmer vs cooler
sea surface
areas as supposed explanations
of climate change neglect all the energy that goes into ocean heat content, melting large
ice deposits and so forth.
These wildfires release soot into the atmosphere, which accelerates the rate
of melting
of glaciers, snow and
ice it lands upon, which can lead to less reflectivity, meaning more
of the sun's heat is absorbed, leading to more
global warming, which leads to even more wildfires, not to mention greater
sea level rise, which is already threatening coastal
areas around the world.
Goddard moves on to a graph, apparently from the University
of Illinois (no cite, but it looks real) showing
global sea ice area from 1979 to the present.
Having said that, it is a really small effect — if the entire Arctic summer
sea ice pack melted (average thickness 2 metres, density ~ 920 kg / m3,
area 3 × 10 ^ 6 km ^ 2 (0.8 % total ocean
area) = > a 4.5 cm rise instantly which implies a
global sea level rise
of 0.36 mm.
If all
of the currently attainable carbon resources [estimated to be between 8500 and 13.600 GtC (4)-RSB- were burned, the Antarctic
Ice Sheet would lose most of its mass, raising global sea level by more than 50 m. For the 125 GtC as well as the 500, 800, 2500, and 5000 GtC scenarios, the ice - covered area is depicted in white (ice - free bedrock in brow
Ice Sheet would lose most
of its mass, raising
global sea level by more than 50 m. For the 125 GtC as well as the 500, 800, 2500, and 5000 GtC scenarios, the
ice - covered area is depicted in white (ice - free bedrock in brow
ice - covered
area is depicted in white (
ice - free bedrock in brow
ice - free bedrock in brown).
Arbetter, 4.7, Statistical A statistical model using regional observations
of sea ice area and
global NCEP air temperature,
sea level pressure, and freezing degree day estimates continues the trend
of projecting below - average summer
sea ice conditions for the Arctic.
Meantime, per Cryosphere, the
Global Sea Ice Area fell by over 1 million km in a matter
of about 5 days.
Translated by Google from this press release in German at the Alfred Wegener Institute in Germany: Never so much
sea ice at Antarctica in the last 30 years In light
of global warming, it seems paradoxical that the
sea ice cover
of the Southern Ocean has covered a larger
area in the past month than...
Global sea levels could rise by more than 20 feet with the loss
of shelf
ice in Greenland and Antarctica, devastating coastal
areas worldwide.
The biggest
area of marine
ice in the east is likely to be released despite the cold air temperatures, confirming the worries about the effect
of melting Antarctic
ice on
global sea levels.
[48] The Cryosphere Today, «
Global Sea -
Ice Area, 1979 - Present,» University
of Illinois Urbana — Champaign, http://arctic.atmos.uiuc.edu/cryosphere/IMAGES/
global.daily.
ice.
area.withtrend.jpg (accessed February 3, 2016).
For example, the dramatic decline
of summer
sea ice in the Arctic — a loss
of ice cover roughly equal to half the
area of the continental United States — exacerbates
global warming by reducing the reflectivity
of Earth's surface and increasing the amount
of heat absorbed.
All
of these characteristics (except for the ocean temperature) have been used in SAR and TAR IPCC (Houghton et al. 1996; 2001) reports for model - data inter-comparison: we considered as tolerable the following intervals for the annual means
of the following climate characteristics which encompass corresponding empirical estimates:
global SAT 13.1 — 14.1 °C (Jones et al. 1999);
area of sea ice in the Northern Hemisphere 6 — 14 mil km2 and in the Southern Hemisphere 6 — 18 mil km2 (Cavalieri et al. 2003); total precipitation rate 2.45 — 3.05 mm / day (Legates 1995); maximum Atlantic northward heat transport 0.5 — 1.5 PW (Ganachaud and Wunsch 2003); maximum
of North Atlantic meridional overturning stream function 15 — 25 Sv (Talley et al. 2003), volume averaged ocean temperature 3 — 5 °C (Levitus 1982).
The small
global mean change, however, is expected to create large problems in sensitive
areas of the Earth system — rising
sea level leading to increased coastal flooding, more heat waves and drought, and the disappearance
of summer Arctic
sea ice, to name a few.
Then, in the beginning days
of February, the Arctic
sea ice extent and
area both broke records again, as the entire
global sea ice area entered the second - lowest range ever to have been recorded.
Mean
sea level (MSL) evolution has a direct impact on coastal
areas and is a crucial index
of climate change since it reflects both the amount
of heat added in the ocean and the mass loss due to land
ice melt (e.g. IPCC, 2013; Dieng et al., 2017) Long - term and inter-annual variations
of the
sea level are observed at
global and regional scales.
Another indicator
of intensifying
global warming: The
area of Arctic Ocean covered by
sea ice, a major influencer
of weather for the Northern Hemisphere, continued its multi-year shrinking trend.
Researchers are still hunting for plausible reasons why the
area of Antarctic
sea ice for May was an above - average 4.64 million square miles (12.03 million square kilometers), according to the NSIDC, despite the multi-year overall increase in
global surface temperatures.
Anomolous
global sea ice area would seem to be over a million square kilometers below the 1979 - 2000 mean... hmmm and continuing lack
of sunspots should mean lower
global temperatures... hmmm
My own view is that the initiating mechanism is not small shifts in insolation hitting some kind
of trigger related to snow albedo (the land -
sea snow -
ice area is relatively small compared to potential shifts in cloud amount and spatial distribution)-- rather it is shifts in
global winds which likely relate to shifts in the jetstream (linked to...?
Unless
global temperatures are stabilized, higher
seas from melting
ice sheets and mountain glaciers, combined with the heat - driven expansion
of ocean water itself, will eventually lead to the displacement
of millions
of people as low - lying coastal
areas and island nations are inundated.
The acceleration
of ice loss in both Greenland and Antarctica has caused another upward revision
of global sea - level rise and the numbers
of refugees expected from low - lying coastal
areas.
Record droughts in many
areas of the world, the loss
of arctic
sea ice — what you see is an increasing trend that is superimposed on annual variablity (no bets on what happens next year, but the five - to - ten year average in
global temperatures,
sea surface temperatures, ocean heat content — those will increase — and
ice sheet volumes, tropical glacier volumes,
sea ice extent will decrease.
pdf cited by Will ««Observed
global sea ice area, defined here as a sum
of N. Hemisphere and S. Hemisphere
sea ice areas, is near or slightly lower than those observed in late 1979.»
Global mass balance data are transformed to
sea - level equivalent by first multiplying the
ice thickness (meters) lost to melting by the density
of ice (about 900 kilograms per cubic meter), to obtain a water equivalent thickness, and then multiplying by the surface
area of these «small» glaciers (about 760,000 square kilometers).
«It is unlikely that coastal cities or low - lying
areas such as Bangladesh, European lowlands, and large portions
of the United States eastern coast and northeast China plains could be protected against such large
sea level rise,» states a report co-authored by Hansen, titled «Ice Melt, Sea Level Rise and Superstorms: Evidence from Paleoclimate Data, Climate Modeling, and Modern Observations that 2 °C Global Warming is Highly Dangerous&raqu
sea level rise,» states a report co-authored by Hansen, titled «
Ice Melt,
Sea Level Rise and Superstorms: Evidence from Paleoclimate Data, Climate Modeling, and Modern Observations that 2 °C Global Warming is Highly Dangerous&raqu
Sea Level Rise and Superstorms: Evidence from Paleoclimate Data, Climate Modeling, and Modern Observations that 2 °C
Global Warming is Highly Dangerous».
The report singles out coastal
areas, including low - lying island nations, as hot spots
of elevated risk that may not be completely manageable due to the steady climb in
global sea levels projected to take place during the rest
of this century, as the planet warms and land - based
ice sheets melt.
For an annual - and
area - average warming exceeding Embedded Image in Greenland and Embedded Image in the
global average, the net surface mass balance
of the Greenland
ice sheet becomes negative, in which case it is likely that the
ice sheet would eventually be eliminated, raising
global - average
sea level by 7 m.