The Sea Ice Index relies on NASA - developed methods to estimate
sea ice conditions using passive - microwave data from the Defense Meteorological Satellite Program (DMSP) the Special Sensor Microwave Imager / Sounder (SSMIS).
Not exact matches
[Andy Revkin — The model runs
used by the U.S. Geological Survey's Steven Amstrup to project
sea ice conditions midcentury onward all presumed carbon dioxide concentrations continue to rise.
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.
This month's report includes details on the causes of the 2012 minimum, the
use of
sea ice volume versus extent,
sea ice in climate models, and late spring 2013
conditions.
«
Using a GCM, can we regenerate the land temperature record from the ocean record using observed SSTs and sea ice distribution as a boundary condi
Using a GCM, can we regenerate the land temperature record from the ocean record
using observed SSTs and sea ice distribution as a boundary condi
using observed SSTs and
sea ice distribution as a boundary
condition?
On the other side of the Arctic, Russian martime operations
using icebreakers on the Northern
Sea Route began in 1932 and give no evidence for improving
ice conditions in this period; rather the opposite, as 1937 and 1940 were noted for heavy
ice in the Laptev
Sea.
The new system — which captures current
sea -
ice conditions more accurately and in greater detail by blending several streams of data — has been
used operationally in Navy forecasting since February, Posey said.
The ARISE campaign,
using NASA's C - 130 Hercules aircraft from Wallops Flight Facility in Virginia, had its first science flight on Sept. 4 and has already carried out several surveys of
sea ice and cloud
conditions.
A regression - based forecast for September
ice extent around Svalbard (an area extending from 72 — 85N and 0 — 40E), which
uses May
sea surface temperatures, the March index of the Arctic Oscillation, and April
ice conditions as predictors, yielded a mean
ice extent in September 2010 of 255,788 square kilometers around Svalbard.
This is substantially lower than the earlier estimates, reflecting both lower than average
sea ice extent
used as initial
conditions this summer and a persistent downward trend in
sea ice extent over the past decade (and longer).
We also make
use of two lengthy control simulations conducted with CESM1 under constant 1850 radiative
conditions: a 2200 - year control run
using the fully - coupled configuration (hereafter termed the «coupled control run»), and a 2600 - year control run
using only the atmospheric model component coupled to the land model component from CESM1 with a specified repeating seasonal cycle of
sea surface temperatures (SSTs) and
sea ice conditions taken from the long - term climatology of the fully - coupled control run (hereafter termed the «atmospheric control run»).
The ensemble consists of seven members each of which
uses a unique set of NCEP / NCAR atmospheric forcing fields from recent years, representing recent climate, such that ensemble member 1
uses 2005 NCEP / NCAR forcing, member 2
uses 2006 forcing..., and member 7
uses 2011 forcing... In addition, the recently available IceBridge and helicopter - based electromagnetic (HEM)
ice thickness quicklook data are assimilated into the initial 12 - category
sea ice thickness distribution fields in order to improve the initial
conditions for the predictions.
Arbetter, 4.0, n / a, Statistical (updated 13 August)
Using conditions from week 30 of 2012 (ie August 1, 2012), a revised minimum Arctic
sea ice extent of 4.03 million km2 is projected for the week of September 7, 2012.
On 27 June 2008 a request was issued to the arctic research community requesting input for the June 2008 Outlook Report on arctic
sea ice conditions for September 2008, to update the May Outlook
using June data.
A smaller multiyear
ice area in the Arctic Ocean means that the
sea ice summer extent is more sensitive to weather
conditions during summer and thus more difficult to predict
using statistical regression analysis since seasonal weather forecasts are not reliable.
However, the ensemble mean September 2008
sea ice conditions,
using the range of historical summer weather, gives a value of
sea ice extent that is slightly more than 2007.
To obtain the «best possible» initial
ice - ocean
conditions for the forecasts, we conducted a retrospective simulation
using PIOMAS that assimilates satellite
ice concentration and
sea surface temperature data.
Our projected Arctic
sea ice extent from the NCEP CFSv2 model with June 2013 revised - initial
condition using 30 - member ensemble forecast is (surprisingly increased to) 4.7 million square kilometers with a standard deviation of 0.4 million square kilometers.
Proxy data such as those generated from
ice core samples, measurements of tree rings intervals, bore samples taken from sediments from the ocean and
sea floor, and measurement of gases from bubbles trapped in
ice are some examples of preserved physical characteristics of the past
used by scientists to reconstruct prevailing climatic
conditions in the past.
As with previous CIS contributions, the 2016 forecast was derived by considering a combination of methods: 1) a qualitative heuristic method based on observed end - of - winter Arctic
ice thickness / extent, as well as winter surface air temperature, spring
ice conditions and the summer temperature forecast; 2) a simple statistical method, Optimal Filtering Based Model (OFBM), that
uses an optimal linear data filter to extrapolate the September
sea ice extent time - series into the future and 3) a Multiple Linear Regression (MLR) prediction system that tests ocean, atmosphere and
sea ice predictors.
The second method
uses a optimal filtering based statistical model, and the third estimate is based on regression models relating September
sea ice extent to spring atmospheric and oceanic
conditions.
When scientists compare average
sea ice conditions between years, they often
use a 30 - year reference period of 1981 to 2010.
Because Arctic
sea ice is influenced by both air and water temperatures, the study authors
use a combination of Arctic
ice core, tree - ring and lake sediments to reconstruct Arctic
conditions over the last 2,000 years.
In their paper «Exploring recent trends in Northern Hemisphere blocking,» Barnes and colleagues
used various meteorological definitions of «blocking» along with various datasets of atmospheric
conditions to assess whether or not there have been any trends in the frequency of blocking events that could be tied to changes in global warming and / or the declines in Arctic
sea ice.
«Polar bears are sticking to
using the same type of habitat
conditions even while
sea ice disappears,» says lead author Ryan Wilson of the U.S. Fish and Wildlife Service.
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.
Using a model that tracked a range of habitat
conditions, including water temperature and depth from
sea ice, to predict which habitats would be most impacted by climate change, William Cheung, the study's lead author, and his colleagues found that around 50 species of commercial fishes living near or at the poles will go extinct within the next 4 decades.
They also ran atmospheric models that
used observed global
sea surface temperatures, Arctic
sea ice conditions and atmospheric carbon dioxide concentrations in 2010 to assess whether such factors might have contributed to the heat wave.
However, scientists have
used historical records of
sea ice conditions to estimate
sea ice extent before 1979.
The passive - microwave data
used for the
Sea Ice Index is especially helpful because the sensor can «see» through clouds and deliver data even during the six months of Arctic darkness and frequently cloudy
conditions.
While several August Outlooks did not change from the July Outlook, forecasts
using statistical techniques together with end of July
sea ice conditions tended to show slightly lower estimates for the September minimum compared to the previous outlook (e.g. Meier et al.; Beitsch et al.; Lukovich et al.; Randles).
Or, to understand the causes of melting
sea -
ice or severe drought, researchers can
use sophisticated climate models to help identify — and potentially isolate — various factors that could individually contribute or dynamically interact to influence climate
conditions in a particular region,» he says.