Networking scientists and stakeholders to improve
sea ice prediction in a changing Arctic.
«Impacts of Assimilating Satellite Sea Ice Concentration and Thickness on Arctic
Sea Ice Prediction in the NCEP Climate Forecast System» J. Climate 0, (https://doi.org/10.1175/JCLI-D-17-0093.1).
Given the lack of meteorological support and several indications that the sea ice was rather thin, we note that thermodynamic melting of thin, mobile sea ice is now a dominant process, justifying the low
sea ice predictions in the Sea Ice Outlook.
Not exact matches
This gives confidence
in the
predictions of the current generation of
ice - sheet models which are used to forecast future
ice loss from Antarctica and resulting
sea - level rise.»
«
Ice loss from this part of West Antarctica is already making a significant contribution to
sea - level rise — around 1 mm per decade, and is actually one of the largest uncertainties
in global
sea - level rise
predictions.
In turn, sharing scientific and indigenous predictive capabilities is meant to improve coastal ice interpretation and prediction based on satellite imagery, assist communities refining public safety measures, and to add local sea ice to parameters used in assessing global climate change in the Arcti
In turn, sharing scientific and indigenous predictive capabilities is meant to improve coastal
ice interpretation and
prediction based on satellite imagery, assist communities refining public safety measures, and to add local
sea ice to parameters used
in assessing global climate change in the Arcti
in assessing global climate change
in the Arcti
in the Arctic.
Given that we now have several years more data, we can essentially «test» the IPCC
predictions and we arrive at the conclusion (i.e., message 1) that the climate system is tracking the «worst case scenario» (or worse
in the case of
ice melt and
sea - level rise) presented by the IPCC.
«We found that
in years when the
sea ice extent departed strongly from the trend, such as
in 2012 and 2013,
predictions failed regardless of the method used to forecast the September
sea ice extent,» said Julienne Stroeve, a senior scientist at NSIDC and professor at University of College London.
The next step is to use estimates of future
sea ice loss to make
predictions of how further melting could influence summer rainfall
in Europe
in the years to come.
At the same time, there is considerable public interest
in dependable
predictions concerning Arctic
sea ice development over the next few decades, so as to have a basis for long - term strategic planning.
Although researchers have been generally successful at modelling the huge declines
in Arctic
sea ice, the extent of Antarctic
sea ice has actually increased
in recent years, contrary to the
predictions of models.
A project off Greenland will tag whales with sensors to measure
sea temperatures and
ice melt
in hard - to - reach places, improving
predictions of
sea - level rise
Better modeling of Arctic
sea -
ice changes could improve
prediction of changes
in rainfall, the researchers said.
Kuhn, from Germany's Alfred Wegener Institute, added, «This gives confidence
in the
predictions of the current generation of
ice sheet models which are used to forecast future
ice loss from Antarctica and resulting
sea - level rise.»
A number of recent studies linking changes
in the North Atlantic ocean circulation to
sea ice extent led Yeager to think that it would also be possible to make decadal
predictions for Arctic winter
sea ice cover using the NCAR - based Community Earth System Model...
Current
predictions [5], [6] suggest that trends
in sea ice extent will alter
in the second half of this century and that the annual average
sea ice extent will diminish by 33 %; most of this retreat is expected to occur
in winter and spring [5], [6], with attendant risks for emperor penguins.
PIOMAS has been run
in a forward mode (and hence without data assimilation) to yield seasonal
predictions for the
sea ice outlook (Zhang et al. 2008) and has also provided input to statistical forecasts (Lindsay et al. 2008) and fully - coupled models.
Prediction methods for the
sea ice minima range from ad - hoc guesses to model
predictions, from statistical analyses to water - cooler speculation
in the blogosphere.
Many of these
predictions are compiled
in the SEARCH - sponsored «
sea ice outlook ``.
For is it not true that the IPCC is comprised of a wide range of scientist and they all must agree on the content of their reports, that some of said scientists are either on the payroll of oil - dependent nations or are politically conservative, and that the IPCC
predictions have consistently underestimated the effects of climate change
in terms of temperature rise,
sea level rise,
ice cap diminution, etc..?
We find a consistent decreasing trend
in Arctic Ocean
sea ice thickness since 1979, and a steady decline
in the Eastern Arctic Ocean over the full 40 - year period of comparison that accelerated after 1980, but the
predictions of Western Arctic Ocean
sea ice thickness between 1962 and 1980 differ substantially.
First is the identification of a runaway condition
in outflow glaciers of the West Antarctic
ice sheet that makes the IPCC
prediction for year - 2100
sea level rise clearly obsolete.
Topics of potential interest: The successful OCO - 2 launch, continuing likelihood of an El Niño event this fall,
predictions of the September Arctic
sea ice minimum, Antarctic
sea ice excursions, stochastic elements
in climate models etc..
«The intent is not to issue
predictions, but rather to summarize all available information from ongoing observing and modeling efforts to provide the scientific community, stakeholders, and the public the best available information on the evolution of the arctic
sea ice cover,» said the coordinators
in a statement.
Taken at face value, Fig 3 manifests into a
prediction that
sea ice will increase, with expected values
in 2080 25 % above 2011 values.
In online science discussions, the fate of this years summer
sea ice has been the focus of a significant betting pool, a test of expert
prediction skills, and a week - by - week (almost) running commentary.
The article
in The Independent makes its
predictions based on the increased speed of reduction of the
Sea Ice Area compared to last year.
You can compare the current
ice conditions with predictions made earlier in the year through the Sea Ice Outlook effort, a project of the Arctic Research Consorti
ice conditions with
predictions made earlier
in the year through the
Sea Ice Outlook effort, a project of the Arctic Research Consorti
Ice Outlook effort, a project of the Arctic Research Consortium.
Interannual variability is prominent
in all regions and will pose a challenge to
sea ice prediction efforts.
Still, there are many other veteran
sea - ice scientists (this is not false balance) who note that the complexity of this system has consistently defied predictions in either direction (see this year's Sea Ice Outlook forecasts to get the range of forecast
sea -
ice scientists (this is not false balance) who note that the complexity of this system has consistently defied predictions in either direction (see this year's Sea Ice Outlook forecasts to get the range of forecast
ice scientists (this is not false balance) who note that the complexity of this system has consistently defied
predictions in either direction (see this year's
Sea Ice Outlook forecasts to get the range of forecast
Sea Ice Outlook forecasts to get the range of forecast
Ice Outlook forecasts to get the range of forecasts).
Even prior to any large feedback involving the
ice sheets or carbon cycle, the actual rise
in sea - level continues to be at the top edge of the envelope of the IPCC's
predictions.
Canadian
Ice Service, 4.7, Multiple Methods As with CIS contributions in June 2009, 2010, and 2011, the 2012 forecast was derived using a combination of three methods: 1) a qualitative heuristic method based on observed end - of - winter arctic ice thicknesses and extents, as well as an examination of Surface Air Temperature (SAT), Sea Level Pressure (SLP) and vector wind anomaly patterns and trends; 2) an experimental Optimal Filtering Based (OFB) Model, which uses an optimal linear data filter to extrapolate NSIDC's September Arctic Ice Extent time series into the future; and 3) an experimental Multiple Linear Regression (MLR) prediction system that tests ocean, atmosphere and sea ice predicto
Ice Service, 4.7, Multiple Methods As with CIS contributions
in June 2009, 2010, and 2011, the 2012 forecast was derived using a combination of three methods: 1) a qualitative heuristic method based on observed end - of - winter arctic
ice thicknesses and extents, as well as an examination of Surface Air Temperature (SAT), Sea Level Pressure (SLP) and vector wind anomaly patterns and trends; 2) an experimental Optimal Filtering Based (OFB) Model, which uses an optimal linear data filter to extrapolate NSIDC's September Arctic Ice Extent time series into the future; and 3) an experimental Multiple Linear Regression (MLR) prediction system that tests ocean, atmosphere and sea ice predicto
ice thicknesses and extents, as well as an examination of Surface Air Temperature (SAT),
Sea Level Pressure (SLP) and vector wind anomaly patterns and trends; 2) an experimental Optimal Filtering Based (OFB) Model, which uses an optimal linear data filter to extrapolate NSIDC's September Arctic Ice Extent time series into the future; and 3) an experimental Multiple Linear Regression (MLR) prediction system that tests ocean, atmosphere and sea ice predicto
Sea Level Pressure (SLP) and vector wind anomaly patterns and trends; 2) an experimental Optimal Filtering Based (OFB) Model, which uses an optimal linear data filter to extrapolate NSIDC's September Arctic
Ice Extent time series into the future; and 3) an experimental Multiple Linear Regression (MLR) prediction system that tests ocean, atmosphere and sea ice predicto
Ice Extent time series into the future; and 3) an experimental Multiple Linear Regression (MLR)
prediction system that tests ocean, atmosphere and
sea ice predicto
sea ice predicto
ice predictors.
Yuan et al. (LDEO Columbia University), 5.08 (+ / - 0.51), Statistical The
prediction is made by statistical models, which are capable to predict Arctic
sea ice concentrations at grid points 3 - month
in advance with reasonable skills.
In late August, a Reuters story began with «a thaw of Antarctic ice is outpacing predictions by the U.N. climate panel and could in the worst case drive up world sea levels by 2 meters (6 feet) by 2100, a leading expert said.&raqu
In late August, a Reuters story began with «a thaw of Antarctic
ice is outpacing
predictions by the U.N. climate panel and could
in the worst case drive up world sea levels by 2 meters (6 feet) by 2100, a leading expert said.&raqu
in the worst case drive up world
sea levels by 2 meters (6 feet) by 2100, a leading expert said.»
During the final months of funding for the initial
Sea Ice Prediction Network (SIPN) project, efforts were focused on the core
Sea Ice Outlook (SIO) activities
in the summer and fall of 2017.
By: Betsy Turner - Bogren and Helen Wiggins, ARCUS SIPN 2017 During the final months of funding for the initial
Sea Ice Prediction Network (SIPN) project, efforts were focused on the core
Sea Ice Outlook (SIO) activities
in the summer and fall of 2017.
I am making no
prediction about long term trends
in sea ice.
Precise weather and
sea -
ice predictions will play an increasingly important role
in managing related safety issues
in polar regions.
The «so called science» has so far proven remarkably accurate
in its
predictions of a warming planet, increasing heat waves, fires, melting
ice caps, loss of
sea ice, species migration and variable rainfall.
The only problem with all the
predictions about the level of the World Ocean rising is that, the World Ocean is refusing to rise up
in support of the
predictions, the other problem is that
ice is frozen fresh water and frozen fresh water only covers about 5 % of this planet above
sea level and frozen water under the level of the World Ocean does not count as the World Ocean will fall a small amount if that
ice melts, so if the
ice there is enough to get the World Ocean to rise and significant amount then it must be piled up very high, I cubic kilometer of water as
ice, should it melt, would make 1000 square kilometers rise by one meter, so when you use this simple math then somewhere on the planet, above the level of the
sea, then there must be over 500,000 cubic kilometers of
ice, piled up and just waiting to melt, strange that no one can find that amount of
ice, all these morons who talk about the rise of the World Ocean
in tens of meters, this includes you Peter Garrett or Mr. 7 Meters, the
ice does not exist to allow this amount of rise
in the World Ocean, it is just not there.
A central topic will be teleconnections
in the climate system, i.e. how a change
in climate
in one part of the globe (e.g. temperatures
in the Atlantic or shrinking
sea ice cover
in the Arctic) can influence climate on other parts of the globe (e.g. Eurasian winter temperatures), and how we can use this information to improve regional climate
prediction and therefore regional climate service.
Chapman, W.L. and J.E. Walsh 1991 Long - Range
Prediction of Regional
Sea Ice Anomalies
in the Arctic Weather and Forecasting 6, 271 - 288.
As the rate of
sea ice decline speeds up it is starting to exceed the
predictions of climate computer models which had previously suggested that by 2100 the Arctic will be
ice free
in summer.
With impacts on Arctic coastal communities and increases
in maritime activities, both observations of changes underway and
predictions at the scale of less than a week to several months out are of importance to the research community and those living and operating
in ice - covered
seas.
Predictions, an early baby El Nino this coming year, 2014, will fade and 2014 will be the 9 nth coldest of recent years Arctic
Sea Ice extent will speed up
in the coming months and go through the average to record a positive anomaly within 12 weeks.
Yet some kind of climate model is indispensable to make future
predictions of the climate system and IPCC has identified several reasons for respect
in the climate models including the fact that models are getting better
in predicting what monitoring evidence is actually observing around the world
in regard to temperature,
ice and snow cover, droughts and floods, and
sea level rise among other things.
The Fall 2017 issue of Witness the Arctic includes news about the NSF Vision for Research Support and Logistics at Summit Stations; Arctic Social Science research on Alaska Native Elderly health;
Sea Ice Prediction Network activities; the Study of Environmental Arctic Change program's syntheses and communication efforts; a workshop on relationships between research and Alaskan Indigenous communities; the newly - released map for the Agreement to Enhance International Arctic Scientific Cooperation; an international workshop on maritime traffic
in the Bering Strait; IARPC and the Polar Research Board activities; the 2017 Joint Science Education Project, international activities at IASC, the Year of Polar
Prediction project, and the Greenland Ecological Monitoring Program; recent ARCUS activities; and comments from ARCUS Executive Director, Robert Rich.
These
sea level change
predictions may be underestimates, however, because they do not account for any increases
in the rate at which the world's major
ice sheets are melting.
If things are so good now, despite declines
in summer
sea ice, what does that say about the accuracy of their
predictions?
A new ensemble
prediction from an
ice - ocean model was submitted by Zhang for the July outlook and the new
sea ice thickness map for September 2010 still shows
ice remaining
in Lancaster Sound.