Full Access On the Robustness of Bayesian Fingerprinting Estimates
of Global Sea Level Change
Not exact matches
We have much better — and more conclusive — evidence for climate
change from more boring sources like
global temperature averages, or the extent
of global sea ice, or thousands
of years» worth
of C02
levels stored frozen in ice cores.
But the study, published today in Earth's Future, finds that scientists won't be able to determine, based on measurements
of large - scale phenomena like
global sea level and Antarctic mass
changes, which scenario the planet faces until the 2060s.
Changes in three important quantities —
global temperature,
sea level and snow cover in the Northern Hemisphere — all show evidence
of warming, although the details vary.
Studying surging glaciers could also offer insights into grander - scale ice flows with
global consequences: the movements
of the ice sheets in Antarctica and Greenland, which can
change abruptly, altering the ice discharges that affect
sea level.
As Congress continues to consider policy options to combat the effects
of sea level rise and climate
change, one thing is clear: There is no silver bullet solution to this
global problem.
Global warming could seriously mess with fisheries in a few ways: Carbon dioxide in the air contributes to ocean acidification,
sea level rise could
change the dynamics
of fisheries, and cold water fish like salmon could be pushed out by warming streams.
An overwhelming majority
of scientists say the burning
of oil, gas and coal is a driver
of global climate
change, causing
sea level rise and more frequent violent storms.
«Until recently, only West Antarctica was considered unstable, but now we know that its ten times bigger counterpart in the East might also be at risk,» says Levermann, who is head
of PIK's research area
Global Adaptation Strategies and a lead - author
of the
sea -
level change chapter of the most recent scientific assessment report by the Intergovernmental Panel on Climate Change,
change chapter
of the most recent scientific assessment report by the Intergovernmental Panel on Climate
Change,
Change, IPCC.
This is a particularly useful region because the oxygen isotopic composition
of the seawater is largely determined by the flow
of water through the Strait
of Gibraltar, which in turn is sensitive to
changes in
global sea level — in a way like the pinching
of a hosepipe.
New research indicates that climate
change has triggered an unstoppable decay
of the West Antarctic Ice Sheet, eventually leading to at least three meters
of global sea level rise
Most
of these severe crises are linked to massive volcanic activity,
global climate
changes and
sea level lowstands.
Subglacial lakes are likely to influence the flow
of the ice sheet, impacting
global sea level change.
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.
Furthermore, unraveling the causes
of sea ice retreat should help us understand the mechanisms behind climate
change on a
global level, which is interrelated to the ice reduction in the Arctic ocean.»
The impacts
of climate
change include
global warming, rising
sea levels, melting glaciers and
sea ice as well as more severe weather events.
These vertical motions
of continents and seafloor cause both local and
global changes in
sea level.
The finding, detailed in the Jan. 22 issue
of the journal Nature, suggests that this process could be important to more accurately modeling how Greenland will respond to climate
change and contribute to the already 8 inches
of global sea level rise since 1900.
Of course, while short - term changes in sea level can be predicted fairly accurately based on the motions of the moon and sun, it is a lot harder predicting the ups and downs of the average global surface temperature — there is a lot of noise, or natural variation, in the syste
Of course, while short - term
changes in
sea level can be predicted fairly accurately based on the motions
of the moon and sun, it is a lot harder predicting the ups and downs of the average global surface temperature — there is a lot of noise, or natural variation, in the syste
of the moon and sun, it is a lot harder predicting the ups and downs
of the average global surface temperature — there is a lot of noise, or natural variation, in the syste
of the average
global surface temperature — there is a lot
of noise, or natural variation, in the syste
of noise, or natural variation, in the system.
The impact
of these events on historical societal development emphasizes the potential economic and social consequences
of a future rise in
sea levels due to
global climate
change, the researchers write in the study recently published in the journal Scientific Reports.
A working group known as PALSEA2 (Paleo constraints on
sea level rise) used past records
of local
change in
sea level and converted them to a
global mean
sea level by predicting how the surface
of the Earth deforms due to
changes in ice - ocean loading
of the crust, along with
changes in gravitational attraction on the ocean surface.
Dr Ohneiser says that one
of the key implications
of the study is that
changes in
global sea -
level are uneven when ice sheets expand or retreat.
Dr Jochen Hinkel from
Global Climate Forum in Germany, who is a co-author
of this paper and a Lead Author
of the coastal chapter for the 2014 IPCC Assessment Report added: «The IPCC has done a great job in bringing together knowledge on climate
change,
sea -
level rise and is potential impacts but now needs to complement this work with a solution - oriented perspective focusing on overcoming barriers to adaptation, mobilising resources, empowering people and discovering opportunities for strengthening coastal resilience in the context
of both climate
change as well as existing coastal challenges and other issues.»
A team headed by R. Steven Nerem
of the Center for Space Research at the University
of Texas at Austin recently concluded that the ENSO induced
changes in
sea level are not confined to the Pacific but effect
sea level on a
global basis.
Aside from its impact on
sea levels, weather and the economy, researchers say climate
change is also an urgent public health concern, a matter that has been largely left out
of the
global climate conversation until recently.
The finding, which will likely boost estimates
of expected
global sea level rise in the future, appears in the March 16 issue
of the journal Nature Climate
Change.
This was compared with historical tide - gauge and satellite observations
of sea -
level change for the «
global warming» period, since the industrial revolution.
Fact # 1: Carbon Dioxide is a Heat - Trapping Gas Fact # 2: We Are Adding More Carbon Dioxide to the Atmosphere All the Time Fact # 3: Temperatures are Rising Fact # 4:
Sea Level is Rising Fact # 5: Climate
Change Can be Natural, but What's Happening Now Can't be Explained by Natural Forces Fact # 6: The Terms «
Global Warming» and «Climate
Change» Are Almost Interchangeable Fact # 7: We Can Already See The Effects
of Climate
Change Fact # 8: Large Regions
of The World Are Seeing a Significant Increase In Extreme Weather Events, Including Torrential Rainstorms, Heat Waves And Droughts Fact # 9: Frost and Snowstorms Will Still Happen in a Warmer World Fact # 10:
Global Warming is a Long - Term Trend; It Doesn't Mean Next Year Will Always Be Warmer Than This Year
«The
global mean
sea level is rising because
of climate
change, but the
change depends on where you are in the world,» says Rüdiger Haas.
The ice that is
of most concern is the West Antarctic Ice Sheet, which is undergoing unprecedented
changes, and is likely the biggest potential player in future
global sea level rise.
Nonetheless, with rising
sea level and environmental refugeeism compounding the increased demand on water, food, and land
of a growing population (albeit one likely to
level out mid 21st century), the combined impacts
of climate
change and
global population increase could potentially yield a world that doesn't look that different from the one portrayed in the movie — indeed, as Jim Hansen puts it, «a different planet» — by century's end.
Axel Timmermann and Tobias Friedrich constructed a numerical model that quantifies the effects
of past climate and
sea -
level change on
global human migration patterns over the past 125,000 years.
Since the 19th century,
sea level has shot up more than 2 millimeters per year on average, far faster than other periods
of global temperature
change.
Current
changes in the ocean around Antarctica are disturbingly close to conditions 14,000 years ago that new research shows may have led to the rapid melting
of Antarctic ice and an abrupt 3 - 4 metre rise in
global sea level.
Combining POLENET measurements
of gravity,
sea level, and the atmosphere will link ice sheet
change to the
global earth system.
... 25 Nov 2005 article in Science, The Phanerozoic Record
of Global Sea -
Level Change (Miller, K.G. et.
Third, using a «semi-empirical» statistical model calibrated to the relationship between temperature and
global sea -
level change over the last 2000 years, we find that, in alternative histories in which the 20th century did not exceed the average temperature over 500-1800 CE,
global sea -
level rise in the 20th century would (with > 95 % probability) have been less than 51 %
of its observed value.
In the Common Era before the 21st century,
changes in ocean heat content and in mountain glaciers were likely the main drivers
of global sea -
level change.
Some studies have attempted to estimate the statistical relationship between temperature and
global sea level seen in the period for which tide gauge records exist (the last 2 - 3 centuries) and then, using geological reconstructions
of past temperature
changes, extrapolate backward («hindcast») past
sea -
level changes.
The IPCC's assessment
of the literature, prior to our study, was that
global sea -
level fluctuations over the last 5 millennia were < ± 25 cm, and that there was no clear evidence
of whether specific fluctuations seen in some regional
sea level records reflected
global changes.
Our new study links a framework for
global and local
sea -
level rise projections with simulations
of two major mechanisms by which climate
change can affect t...
Mitrovica, J. X., Tamisiea, M. E., Davis, J. L. & Milne, G. A. Recent mass balance
of polar ice sheets inferred from patterns
of global sea -
level change.
This study links a framework for
global and local
sea -
level rise projections with simulations
of two major mechanisms by which climate
change can affect the vast Antarctic ice sheet.
This implies that large - scale observations — for example,
of global mean
sea -
level change or
of the
change mass
of the Antarctic ice sheet — will not on their own significantly narrow the range
of late - century
sea -
level projections for decades to come.
Mysterious under - snow lakes pockmarking its edges and deep layers
of ice at higher elevations both point to
changes that could hasten melt and send water cascading into the ocean, pushing
global sea levels ever higher.
Our new study, published today in the journal Earth's Future, finds that — at least from measurements
of global sea level and continental - scale Antarctic ice - sheet
changes — scientists won't be able to tell which road the planet is on until the 2060s.
A large ensemble
of Earth system model simulations, constrained by geological and historical observations
of past climate
change, demonstrates our self ‐ adjusting mitigation approach for a range
of climate stabilization targets ranging from 1.5 to 4.5 °C, and generates AMP scenarios up to year 2300 for surface warming, carbon emissions, atmospheric CO2,
global mean
sea level, and surface ocean acidification.
First, the rate
of global sea -
level change in the 20th century (1.4 ± 0.2 mm / yr) was, with 95 % probability, faster than during any century since at least 800 BCE.
The rate
of change of the theoretical mean
sea level from year to year is not constant either, due to changing rate of the global sea level rise and changes in the Baltic Sea water balan
sea level from year to year is not constant either, due to
changing rate
of the
global sea level rise and changes in the Baltic Sea water balan
sea level rise and
changes in the Baltic
Sea water balan
Sea water balance.
Using a statistical model calibrated to the relationship between
global mean temperature and rates
of GSL
change over this time period, we are assessing the human role in historic
sea -
level rise and identifying human «fingerprints» on coastal flood events.