PI,
Sea Ice Concentration Climate Data Record Sustainment, Enhancement, and Production of Value - Added Products through the Sea Ice Index (NOAA)
Global
sea ice concentration climate data records 1978 - 2015 (v1.2, 2015), [Online].
Not exact matches
The AMO is likely to be a driver of multi-decadal variations in Sahel droughts, precipitation in the Caribbean, summer
climate of both North America and Europe,
sea ice concentration in the Greenland Sea and sea level pressure over the southern USA, the North Atlantic and southern Europe (e.g., Venegas and Mysak, 2000; Goldenberg et al., 2001; Sutton and Hodson, 2005; Trenberth and Shea, 200
sea ice concentration in the Greenland
Sea and sea level pressure over the southern USA, the North Atlantic and southern Europe (e.g., Venegas and Mysak, 2000; Goldenberg et al., 2001; Sutton and Hodson, 2005; Trenberth and Shea, 200
Sea and
sea level pressure over the southern USA, the North Atlantic and southern Europe (e.g., Venegas and Mysak, 2000; Goldenberg et al., 2001; Sutton and Hodson, 2005; Trenberth and Shea, 200
sea level pressure over the southern USA, the North Atlantic and southern Europe (e.g., Venegas and Mysak, 2000; Goldenberg et al., 2001; Sutton and Hodson, 2005; Trenberth and Shea, 2006).
This finding is consistent with the expected effect of increasing greenhouse gas
concentrations and with other observed evidence of a changing
climate such as reductions in Arctic
sea ice extent, melting permafrost, rising
sea levels, and increases in heavy downpours and heat waves.
The laws of physics require that continually increasing GHG
concentrations will mean a continually increasing temperature (subject to the natural
climate fluctuations of course), and that will mean continuing
sea ice decline.
Alarmed at the pace of change to our Earth caused by human - induced
climate change, including accelerating melting and loss of
ice from Greenland, the Himalayas and Antarctica, acidification of the world's oceans due to rising CO2
concentrations, increasingly intense tropical cyclones, more damaging and intense drought and floods, including glacial lakes outburst loods, in many regions and higher levels of
sea - level rise than estimated just a few years ago, risks changing the face of the planet and threatening coastal cities, low lying areas, mountainous regions and vulnerable countries the world over,
The papers questioned everything from the relative role of natural mechanisms in changes to the
climate system vis - à - vis increased CO2
concentrations, the allegedly «unprecedented» nature of modern
climate phenomena such as warming,
sea levels, glacier and
sea ice retreat, and the efficacy and reliability of computer
climate models for projecting future
climate states.
Climate alarm depends on several gloomy assumptions — about how fast emissions will increase, how fast atmospheric concentrations will rise, how much global temperatures will rise, how warming will affect ice sheet dynamics and sea - level rise, how warming will affect weather patterns, how the latter will affect agriculture and other economic activities, and how all climate change impacts will affect public health and w
Climate alarm depends on several gloomy assumptions — about how fast emissions will increase, how fast atmospheric
concentrations will rise, how much global temperatures will rise, how warming will affect
ice sheet dynamics and
sea - level rise, how warming will affect weather patterns, how the latter will affect agriculture and other economic activities, and how all
climate change impacts will affect public health and w
climate change impacts will affect public health and welfare.
WMO will issue its full Statement on the State of the
Climate in 2017 in March which will provide a comprehensive overview of temperature variability and trends, high - impact events, and long - term indicators of climate change such as increasing carbon dioxide concentrations, Arctic and Antarctic sea ice, sea level rise and ocean acidifi
Climate in 2017 in March which will provide a comprehensive overview of temperature variability and trends, high - impact events, and long - term indicators of
climate change such as increasing carbon dioxide concentrations, Arctic and Antarctic sea ice, sea level rise and ocean acidifi
climate change such as increasing carbon dioxide
concentrations, Arctic and Antarctic
sea ice,
sea level rise and ocean acidification.
With global GHG emissions and
concentrations continuing to increase; with
climate change intensifying changes in ecosystems,
ice sheet deterioration, and
sea level rise; and with fossil fuels providing more than 80 % of the world's energy, the likelihood seems low that cooperative actions will prevent increasingly disruptive
climate change over the next several decades.
Determining the mechanisms and feedbacks involved in
climate change at the end of the last
ice age therefore requires an understanding of the relationship between the southern margin
ice retreat and connected meltwater events to atmospheric and
sea surface temperatures,
ice - rafting Heinrich events,
sea level rise, and atmospheric greenhouse gas
concentrations.
The vulnerable nations declared that they are, «Alarmed at the pace of change to our Earth caused by human - induced
climate change, including accelerating melting and loss of
ice from Greenland, the Himalayas and Antarctica, acidification of the world's oceans due to rising CO2
concentrations, increasingly intense tropical cyclones, more damaging and intense drought and floods, including Glacial Lakes Outburst Floods, in many regions and higher levels of
sea - level rise than estimated just a few years ago, risks changing the face of the planet and threatening coastal cities, low lying areas, mountainous regions and vulnerable countries the world over...»
The EUMETSAT Ocean and
Sea Ice Satellite Application Facility (OSI SAF) team is pleased to announce the release of OSI - 450, a new full reprocessing of its
Sea Ice Concentration (SIC)
Climate Data Record (CDR).
In addition, he discussed the increase of atmospheric greenhouse gas
concentrations and the consequent anthropogenic warming of the
climate system, decrease in
sea ice and increase in ocean acidity.
The IPCC 2007 Fourth Assessment of
climate change science concluded that large reductions in the emissions of greenhouse gases, principally CO2, are needed soon to slow the increase of atmospheric
concentrations, and avoid reaching unacceptable levels.However,
climate change is happening even faster than previously estimated; global CO2 emissions since 2000 have been higher than even the highest predictions, Arctic
sea ice has been melting at rates much faster than predicted, and the rise in the
sea level has become more rapid.
In order to test and approve
climate models for simulation and prediction of Arctic
climate and
sea ice cover8, 20,21,22,23,24,25,26,27,28, however, precise (semi-quantitative) proxy records about past
sea ice concentrations are needed.
The «Temperature Departure From Average» map below further reveals the areas of
concentration for
climate engineering orchestrated chemical cool - downs and
sea surface chemical
ice nucleation (also fueling extreme hail events).
Wang, 5.0 (± 0.27), Modeling A projected September Arctic
sea ice extent of 5.0 million km2 is based on a NCEP ensemble mean CFSv2 forecast initialized from the NCEP
Climate Forecast System Reanalysis (CFSR) that assimilates observed
sea ice concentrations and other atmospheric and oceanic observations.
«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).
The AMO is likely to be a driver of multi-decadal variations in Sahel droughts, precipitation in the Caribbean, summer
climate of both North America and Europe,
sea ice concentration in the Greenland Sea and sea level pressure over the southern USA, the North Atlantic and southern Europe (e.g., Venegas and Mysak, 2000; Goldenberg et al., 2001; Sutton and Hodson, 2005; Trenberth and Shea, 200
sea ice concentration in the Greenland
Sea and sea level pressure over the southern USA, the North Atlantic and southern Europe (e.g., Venegas and Mysak, 2000; Goldenberg et al., 2001; Sutton and Hodson, 2005; Trenberth and Shea, 200
Sea and
sea level pressure over the southern USA, the North Atlantic and southern Europe (e.g., Venegas and Mysak, 2000; Goldenberg et al., 2001; Sutton and Hodson, 2005; Trenberth and Shea, 200
sea level pressure over the southern USA, the North Atlantic and southern Europe (e.g., Venegas and Mysak, 2000; Goldenberg et al., 2001; Sutton and Hodson, 2005; Trenberth and Shea, 2006).
The examination of variability ranging from seasonal to interdecadal scales, and of trends within the
climate patterns and total Antarctic
sea ice concentration (SIC) for the 32 — yr period (1982 — 2013) are the key focuses of this paper.
Other
climate or
climate - related variables of importance may include CO2
concentration,
sea -
ice extent, mean
sea level pressure,
sea level, and storm surge frequencies.
Walt Meier Research Scientist, Cryospheric Sciences Lab, NASA Goddard Space Flight Center Specialties:
Sea ice remote sensing; changes in sea ice concentration, extent, motion, thickness and age; development of sea ice climate data records; interaction of sea ice and clim
Sea ice remote sensing; changes in
sea ice concentration, extent, motion, thickness and age; development of sea ice climate data records; interaction of sea ice and clim
sea ice concentration, extent, motion, thickness and age; development of
sea ice climate data records; interaction of sea ice and clim
sea ice climate data records; interaction of
sea ice and clim
sea ice and
climate
NOAA / NSIDC
Climate Data Record of Passive Microwave
Sea Ice Concentration, Boulder, Colorado USA: National Snow and
Ice Data Center.
The strong poleward atmospheric heat and moisture transport may be one reason why the West Antarctic and Peninsula
climate appears to be more strongly coupled with regional
sea ice concentration and extent anomalies than does the East Antarctic (e.g. Jacobs and Comiso 1997; Weatherly et al. 1991).
NOAA@NSIDC is pleased to announce the release of Version 3 Revision 1 of the NOAA / NSIDC
Climate Data Record of Passive Microwave
Sea Ice Concentration data product.
As
concentrations of atmospheric greenhouse gases increase and the
climate warms, it is expected that there will be increased precipitation in mid-latitudes and less formation of
sea ice.
In the new study, published today in Environmental Research Letters, researchers from Russia used
climate models of
sea - ice concentrations to predict what will happen to one optimal trade route along the Northern Sea Route in the futu
sea -
ice concentrations to predict what will happen to one optimal trade route along the Northern
Sea Route in the futu
Sea Route in the future.
Presenting such alternative figures confuses and undermines the public understanding of the actual science, which is an understanding about the driving mechanisms of
sea level rise: thermal expansion of ocean water, melting of mountain glaciers and complex dynamics of large
ice sheets — in correspondence again with projected temperature rise, that is in turn a product of projected rises of greenhouse gas
concentrations using calculated estimates of
climate sensitivity, together creating a net disturbance in Earth's energy balance, the very root cause of anthropogenic
climate change.
The Statement also highlighted that long - term indicators of
climate change such as increasing carbon dioxide
concentrations,
sea level rise and ocean acidification continue «unabated», with Arctic
sea ice coverage remaining below average and the previously stable Antarctic
sea ice extent at or near a record low.
Scientific confidence of the occurrence of
climate change include, for example, that over at least the last 50 years there have been increases in the atmospheric
concentration of CO2; increased nitrogen and soot (black carbon) deposition; changes in the surface heat and moisture fluxes over land; increases in lower tropospheric and upper ocean temperatures and ocean heat content; the elevation of
sea level; and a large decrease in summer Arctic
sea ice coverage and a modest increase in Antarctic
sea ice coverage.
The black line is a simulated mean
sea ice concentration from the CanESM2 large ensemble, a group of models developed at the Canadian Center for
Climate Modelling and Analysis.
For the «2013 as observed» experiment, the atmospheric model uses observed
sea surface temperature data from December 2012 to November 2013 from the Operational Sea Surface Temperature and Sea Ice Analysis (OSTIA) dataset (Stark et al. 2007; Donlon et al. 2012) and present day atmospheric gas concentrations to simulate weather events that are possible given the observed climate conditio
sea surface temperature data from December 2012 to November 2013 from the Operational
Sea Surface Temperature and Sea Ice Analysis (OSTIA) dataset (Stark et al. 2007; Donlon et al. 2012) and present day atmospheric gas concentrations to simulate weather events that are possible given the observed climate conditio
Sea Surface Temperature and
Sea Ice Analysis (OSTIA) dataset (Stark et al. 2007; Donlon et al. 2012) and present day atmospheric gas concentrations to simulate weather events that are possible given the observed climate conditio
Sea Ice Analysis (OSTIA) dataset (Stark et al. 2007; Donlon et al. 2012) and present day atmospheric gas
concentrations to simulate weather events that are possible given the observed
climate conditions.
Consider, for example, that Lowe, et al. [in Avoiding Dangerous
Climate Change, H.J. Schellnhuber et al. (eds), Cambridge University Press, Cambridge, 2006, p. 32 - 33], based on a «pessimistic, but plausible, scenario in which atmospheric carbon dioxide
concentrations were stabilised at four times pre-industrial levels,» estimated that a collapse of the Greenland
Ice Sheet would over the next 1,000 years raise
sea level by 2.3 meters (with a peak rate of 0.5 mm / yr).
A robust feature of the response of
climate models to increases in atmospheric
concentrations of greenhouse gases is the poleward retreat of terrestrial snow and
sea ice, and the polar amplification of increases in lower - tropospheric temperature.
As Media Matters has noted, the IPCC's 2007 «Synthesis Report» concluded that» [w] arming of the
climate system is unequivocal, as is now evident from observations of increases in global average air and ocean temperatures, widespread melting of snow and
ice and rising global average
sea level» and that» [m] ost of the observed increase in global average temperatures since the mid-20th century is very likely [defined in the report as a» > 90 %» probability] due to the observed increase in anthropogenic [human - caused] GHG [greenhouse gas]
concentrations.»
Easterbrook criticized Gore's claims that the melting of
ice sheets in Greenland and Antarctica could lead to substantial increases in
sea levels, that the
concentration of carbon dioxide in the atmosphere is increasing, and that Bush administration officials have attempted to tamper with official reports on the threat posed by
climate change.
A synthetic aperture radar or equivalent capability is also needed in the production of the
sea -
ice climate data record for validation of
sea ice concentration and edge.
With MIS delayed until NPOESS C2, there is a need to continue the long (28 - year)
climate data record of
sea ice extent and
concentration collected by passive microwave radiometers; continued scatterometer and altimeter measurements are also required.
Holds the high correlation among the variables composing these changes — temperature, precipitation, cloudiness,
sea level pressure (SLP), and
ice concentration — suggests that their close coupling collectively represents a fingerprint of Arctic
climate change
Figure 1: A NOAA Geophysical Fluid Dynamics Laboratory
climate model simulation shows a dramatic decrease in late summer Arctic
sea ice concentrations by 2085.