The sea
ice extent measure is broader, including areas of ocean where ice covers 15 % of the surface area.
These meridional patterns delivered substantial record heat to the Arctic, contributing to record low sea
ice extent measures by end of month.
Kaleschke, 4.6 (± 0.9), Statistical I provide a simple statistical estimate for the September sea ice extent based on the total sea
ice extent measured on July 11: 4.6 ± 0.9.
Not exact matches
Since there are many techniques to
measure the MPP, we can keep using its drift to gauge the
extent of
ice - sheet melting — even in between the end of the ageing GRACE mission and the launch of the next generation of gravity -
measuring satellites, says Chen.
Satellites first began
measuring the
extent of sea
ice in the Arctic Ocean during the 1970s.
Since the MPP can be accurately
measured using multiple independent techniques, its position and drift can be used to gauge the
extent of
ice sheet melting, especially in between the end of the ageing GRACE mission and the launch of the next generation of gravity - field -
measuring satellites, says Chen.
CryoSat - 2 carries a radar altimeter optimized to
measure the
extent and thickness of polar
ice.
The Arctic's sea
ice maximum
extent has dropped by an average of 2.8 percent per decade since 1979, the year satellites started
measuring sea
ice.
We've been able to accurately
measure the
extent of Arctic sea
ice from satellites since 1979.
Scientists have used satellites to
measure the
extent of Arctic sea
ice for the past 39 years.
The global mean temperature rise of less than 1 degree C in the past century does not seem like much, but it is associated with a winter temperature rise of 3 to 4 degrees C over most of the Arctic in the past 20 years, unprecedented loss of
ice from all the tropical glaciers, a decrease of 15 to 20 % in late summer sea
ice extent, rising sealevel, and a host of other
measured signs of anomalous and rapid climate change.
While
extent is a traditional
measure of sea
ice, volume is also important.
Just look at the plots taken from CMIP4 and CMIP5 models when they are compared with
measured extents from NSIDC data then tell us where you would place your bet for a summer free of sea
ice.
The motivation for this time series is to visualize the fact that the long term Arctic - wide loss of sea
ice is not only happening in
extent, which is well
measured by satellites, but also in thickness, which isn't.
We know the the areal
extent of sea
ice is an important
measure of the degree of cold in the Arctic Ocean / sea
ice subsystem of Earth's climate but is it not true that even if areal
extent was to increase the amount of
ice could still be much decreased?
In case this isn't already clear, there is simply no
measure — neither thickness nor areal
extent — by which Greenland can be said to have lost 15 % of its
ice.
Sea
ice extent, Greenland Ice Sheet melt extent are additional measures that are exceeding model expectatio
ice extent, Greenland
Ice Sheet melt extent are additional measures that are exceeding model expectatio
Ice Sheet melt
extent are additional
measures that are exceeding model expectations.
Same goes for
measuring sea level, not to mention sea
ice extent, glacial melt, etc..
... the confusion came most likely from a confusion in definitions of what is the permanent
ice sheet, and what are glaciers, with the «glaciers» being either dropped from the Atlas entirely or colored brown (instead of white)... there is simply no
measure — neither thickness nor areal
extent — by which Greenland can be said to have lost 15 % of its
ice.
Just look at the plots taken from CMIP4 and CMIP5 models when they are compared with
measured extents from NSIDC data then tell us where you would place your bet for a summer free of sea
ice.
There is a fascination (maybe obsession) with
measure of
ice melt
extent with virtually no discussion or concern about the impact of an
ice - free Arctic on precip and temp in western North America.
There are two ways to categorize the amount of
ice: by
measuring the
extent (essentially the area of the ocean covered by
ice, though in detail it's a little more complicated) or using volume, which includes the thickness of the
ice.
The Barnett
Ice Severity (BIS) index provides a measure of the extent of open water and the duration of the shipping season as defined by the presence of ice near Barrow, Alaska and onward to Prudhoe B
Ice Severity (BIS) index provides a
measure of the
extent of open water and the duration of the shipping season as defined by the presence of
ice near Barrow, Alaska and onward to Prudhoe B
ice near Barrow, Alaska and onward to Prudhoe Bay.
Scientists use the summer minimum as one
measure of the
extent of Arctic sea
ice for that year.
This is why
extent is such a useful
measure: it only needs observations at the
ice margin, and is robust even with sparse observations.
If you
measure the latitude of the
ice margin at just one point, you can make a very reasonable estimate of the total
extent.
One of the confusing issues that newbies run into is the distinction between the various
measures of arctic
ice, including «area» vs «
extent».
In 1979, when satellites first
measured it, September Arctic sea
ice extent was roughly equivalent to the area of Australia.
Michaels pointed to record Antarctic
ice, which «is at its highest extent measured by the current microwave satellite sounding system» since 1978, according to data from the University of Illinois» Polar Ice Research Cent
ice, which «is at its highest
extent measured by the current microwave satellite sounding system» since 1978, according to data from the University of Illinois» Polar
Ice Research Cent
Ice Research Center.
Another conclusion is that when we weren't accurately
measuring the Antarctic
ice extent it was seen to be «decreasing» and when we started
measuring the Antarctic
ice extent accurately, it wasn't.
Both these
measures put 2011 as the second lowest on record and this year's
ice extent was 938,000 square miles below the average from the period 1979 to 2000.
Antarctic
ice extent setting new records last year, and close to breaking them this year again Extreme weather as
measured by ACE on a decline for decades Drought as
measured by Palmer Drought Index flat for decades Sea level increases not accelerating and possibly starting to decelerate Signature tropospheric hot spot completely missing Scientists by the bushel coming up with some of the most absurd excuses as to why....
For example, let's say that evidence convinced me (in a way that I wasn't convinced previously) that all recent changes in land surface temperatures and sea surface temperatures and atmospheric temperatures and deep sea temperatures and sea
ice extent and sea
ice volume and sea
ice density and moisture content in the air and cloud coverage and rainfall and
measures of extreme weather were all directly tied to internal natural variability, and that I can now see that as the result of a statistical modeling of the trends as associated with natural phenomena.
The warm Arctic winter limited the formation of sea
ice so much that this year's maximum
extent,
measured in March, was the smallest maximum ever recorded.
Stroeve says a couple of powerful cyclones that churned around the high Arctic last month moved sea
ice around and complicated efforts to
measure its
extent.
Arctic sea
ice extent has been
measured by satellites since the 1970s.
The Barnett
Ice Severity (BIS) Index provides a measure of the extent of open water and the duration of the shipping season as defined by the presence of ice near Barrow, Alaska and onward to Prudhoe B
Ice Severity (BIS) Index provides a
measure of the
extent of open water and the duration of the shipping season as defined by the presence of
ice near Barrow, Alaska and onward to Prudhoe B
ice near Barrow, Alaska and onward to Prudhoe Bay.
Cross-validation skill,
measured by the correlation between two - month lead predictions and observations of September
ice extent, is 0.82, while the RMS error of predictions is 0.72 million square km.
The degree to which this estimate is wrong is a
measure of the degree to which the sea
ice extent is not following a linear trend.
Only in this way is the energy balance determined empirically and the multitude of changes — cloud height and
extent, water vapour, ozone, surface temperature,
ice and snow, biology, aerosols — integrated in a comprehensible
measure.
NSIDC scientist Julienne Stroeve travels to the Arctic Ocean to study sea
ice at its lowest
extent since satellites started
measuring it in 1979.
I see, by that logic would you agree that Antarctica has lost
ice dramatically when last summer marked the lowest
ice extent ever
measured in most lifetimes of those of who are involved
measuring this?
Current conditions at the winter maximum (at 17 March 2018, from NSIDC Masie,
extent measured at 14.7 mkm2, using software able to discern more
ice than used for the figures in Table 1), shown below: Continue reading →
Meanwhile, up in the Arctic, distressing new information from the US National Snow and
Ice Data Center in Boulder, Colorado, shows that Arctic sea ice extent has settled to its fourth - lowest level ever measured at the end of the most recent melt seas
Ice Data Center in Boulder, Colorado, shows that Arctic sea
ice extent has settled to its fourth - lowest level ever measured at the end of the most recent melt seas
ice extent has settled to its fourth - lowest level ever
measured at the end of the most recent melt season.
Over the past quarter - century, both the
extent of melting and the length of the melt season on the Greenland
ice sheet have been growing, as local temperatures have risen.6 Satellites
measure the
extent of melting by differentiating between areas of the
ice mass that are fully frozen and those with surface meltwater.
I think someone is confused and unless someone can show me that measurements of fast
ice area or
extent are
measured and published, Steve Mosher has a point.
Cross-validation skill,
measured by correlation between four - month lead prediction and observation of September
ice extent, is 0.77.
A new study published in Nature Geoscience details how analysts were able to estimate the
extent of Greenland's sub-surface
ice despite the fact that conventional radar pinging and satellite readings are incapable of
measuring to great depths along the icy coast.
The orange line marks the median
extent of the
ice from 1979 to 2000 as
measured on September 9 of each of those years.
When, last year, we asked the NSIDC's Walt Meier why the center chose to present data showing only one of the two
measures of Arctic
ice cover that they collect (respectively known as «
extent» and «area»), when the presentation of both would perhaps reflect more realistically the complexity involved in taking such measurements (let alone using them to make predictions,), he told us: