Climate Science News

[Jason-3]The Jason-3 spacecraft entered safe mode on Saturday, April 6, 2019 at 23:17:22 UTC

AVISO Climate Change News - Tue, 2019-04-09 01:26
The Jason-3 spacecraft entered safe mode on Saturday, April 6, 2019 at 23:17:22 UTC, immediately interrupting its measurements. SEALEVEL j3 datasets in NRT are no longer updated with fresh data up to the recovery of the mission.   Investigation in progress on CNES side, the root cause has not yet been identified.
Categories: Climate Science News

April 2019: Pantanal wetlands

AVISO Climate Change News - Wed, 2019-04-03 01:00
Swot will enable to see both the temporal variations and the spatial complexity of the Pantanal...
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Spring arrives in the Arctic

NSIDC Artic Sea Ice News - Wed, 2019-04-03 00:00

Arctic sea ice extent appears to have reached its maximum extent on March 13, marking the beginning of the sea ice melt season. Since the maximum, sea ice extent has been tracking at record low levels. In the Bering Sea, extent increased through the middle of March after setting record lows—only to drop sharply again.

Overview of conditions  National Snow and Ice Data Center|High-resolution image

Figure 1. Arctic sea ice extent for March 2019 was 14.55 million square kilometers (5.62 million square miles). The magenta line shows the 1981 to 2010 average extent for that month. Sea Ice Index data. About the data

Credit: National Snow and Ice Data Center
High-resolution image

Arctic sea ice extent for March averaged 14.55 million square kilometers (5.62 million square miles), tying with 2011 for the seventh lowest extent in the 40-year satellite record. This is 880,000 square kilometers (340,000 square miles) below the 1981 to 2010 average and 260,000 square kilometers (100,400 square miles) above the lowest March average, which occurred in 2017.

The Bering Sea, which had been nearly ice free at the beginning of March, saw gains in extent through the middle of the month. However, those gains were short lived as extent dropped sharply during the last week of March. The Bering Sea typically reaches its maximum ice extent in late March or early April. This year, the maximum occurred in late January and was 34.5 percent below the 1981 to 2010 average maximum. These late-March sea ice extent losses in the Bering Sea accelerated the decline of total Arctic sea ice extent. By April 1, Arctic extent was at a record low for that date.

Other signs of spring are emerging. A substantial amount of ice retreated in the Gulf of St. Lawrence and the Sea of Okhotsk, as well as in the Barents Sea. Late in the month, small areas of open water were observed in sea ice fields from the University of Bremen, particularly near the shores of the Laptev and Kara Seas, the Sea of Okhotsk, and off of northwestern Alaska.

Conditions in context  National Snow and Ice Data Center|High-resolution image

Figure 2a. The graph above shows Arctic sea ice extent as of April 2, 2019, along with daily ice extent data for four previous years and the record low year. 2018 to 2019 is shown in blue, 2017 to 2018 in green, 2016 to 2017 in orange, 2015 to 2016 in brown, 2014 to 2015 in purple, and 2011 to 2012 in dotted brown. The 1981 to 2010 median is in dark gray. The gray areas around the median line show the interquartile and interdecile ranges of the data. Sea Ice Index data.

Credit: National Snow and Ice Data Center
High-resolution image

 NSIDC courtesy NOAA Earth System Research Laboratory Physical Sciences Division| High-resolution image

Figure 2b. This plot shows the departure from average air temperature in the Arctic at the 925 hPa level, in degrees Celsius, for March 2019. Yellows and reds indicate higher than average temperatures; blues and purples indicate lower than average temperatures.

Credit: NSIDC courtesy NOAA Earth System Research Laboratory Physical Sciences Division
High-resolution image

Overall, Arctic weather in March featured low pressure and above average temperatures. Two low pressure centers at sea level, one over the Bering Sea and the other over the Barents Sea, dominated the atmospheric circulation pattern. Low pressure over the Barents Sea brought cloudy and cool conditions to the immediate region, but also funneled warm air into the central Arctic Ocean. Air temperatures at the 925 mb level (about 2500 feet above sea level) were above average over most of the Arctic region, with the exception in the Atlantic sector of the Arctic Ocean. Temperatures were far above average, locally exceeding 10  degrees Celsius (18 degrees Fahrenheit), over the Beaufort Sea, northeast Alaska, and northwest Canada.

The pattern of overall low pressure across the Arctic in March was manifested as a persistent positive phase of the Arctic Oscillation (AO), a pattern that started during the second week of February. A positive AO in winter has in the past favored low September ice extent. This is in part due to a wind pattern tending to advect older, thicker ice out of the Arctic through the Fram Strait. The wind pattern associated with the positive AO also tends to pull ice away from the Siberian coast, resulting in thinner ice in the region that readily melts out during summer. However, with the overall thinning of the Arctic ice cover, the relationship between winter AO phase and September sea ice extent is not as clear as it used to be.

March 2019 compared to previous years  National Snow and Ice Data Center| High-resolution image

Figure 3. Monthly March ice extent for 1979 to 2019 shows a decline of 2.7 percent per decade.

Credit: National Snow and Ice Data Center
High-resolution image

The net change in sea ice extent between the beginning and end of March was small, which is typical for the month. Sea ice extent increased during the first part of the month to the annual maximum on March 13 and then declined through the remainder of the month.

The 1979 to 2019 linear rate of decline for March ice extent is 41,700 square kilometers (16,100 square miles) per year, or 2.7 percent per decade relative to the 1981 to 2010 average.

Winter recap  NSIDC courtesy NOAA Earth System Research Laboratory Physical Sciences Division| High-resolution image

Figure 4. This plot shows average sea level pressure in the Arctic in millibars (hPa) from December 1, 2018 to March 31, 2019. Yellows and reds indicate high air pressure; blues and purples indicate low pressure.

Credit: NSIDC courtesy NOAA Earth System Research Laboratory Physical Sciences Division
High-resolution image

Moderation marked the 2018 to 2019 winter. Air temperatures at the 925 mb level were average to slightly above average over most of the Arctic Ocean, with only the southern Beaufort Sea being especially warm with temperatures 5 degrees Celsius (9 degrees Fahrenheit) higher than average.

Below average pressures at sea level dominated over the Bering Sea and much of the Eurasian side of the Arctic Ocean (Figure 4). Circulation patterns, however, were not especially unusual and there were no pronounced short-term heat waves of the type observed in recent winters. For much of the Arctic, sea ice extent was near average through most of the winter. As noted in a previous post, the most compelling feature of the winter was the substantial ice loss during February and early March in the Bering Sea, leading to nearly ice-free conditions.

Snow on sea ice This graph shows the annual volume of snow on sea ice from 1981 to 2016 based on reanalysis fields from NASA Modern-Era Retrospective analysis for Research and Applications (MERRA-2) (blue) and European Centre for Medium-Range Weather Forecasts (ECMWF) ERA-1 (green).

Figure 5a. This graph shows the annual volume of snow on sea ice from 1981 to 2016 based on reanalysis fields from NASA Modern-Era Retrospective analysis for Research and Applications-2 (MERRA-2) in blue and the European Centre for Medium-Range Weather Forecasts (ECMWF) ERA-Intermin (ERA-I) in green.

Credit: J. Stroeve, NSIDC
High-resolution image

Figure 5b. The top map of the Arctic shows April trends in snow depth (in centimeters/year) from 1981 to 2016 based on NASA Modern-Era Retrospective analysis for Research and Applications-2 (MERRA-2). The bottom map of the Arctic shows April trends in snow depth (in centimeters/year) from 1981 to 2016 based on the European Centre for Medium-Range Weather Forecasts (ECMWF) ERA-Interim (ERA-I). The total volume of accumulation is measured from August through July, starting in the 1980 to 1981 winter. ||Credit: Stroeve et al., 2019 Journal of Geophysical Research-Oceans| High-resolution image

Figure 5b. The top map of the Arctic shows April trends in snow depth (in centimeters/year) from 1981 to 2016 based on NASA Modern-Era Retrospective analysis for Research and Applications-2 (MERRA-2). The bottom map of the Arctic shows April trends in snow depth (in centimeters/year) from 1981 to 2016 based on the European Centre for Medium-Range Weather Forecasts (ECMWF) ERA-Interim (ERA-I). The total volume of accumulation is measured from August through July, starting in the 1980 to 1981 winter.

Credit: Stroeve et al., 2019, Journal of Geophysical Research-Oceans
High-resolution image

With a general trend toward later sea ice formation in autumn and winter and earlier melt in spring and summer, the time period for snow accumulation on the sea ice is changing. However, snow on sea ice is something that satellites do not measure well. As a result, several different approaches have been used to assess snow on sea ice, ranging from using atmospheric reanalysis precipitation forecasts and applying simple temperature thresholds to simulating physical processes impacting snow on sea ice (e.g., wind redistribution, melt, snow compaction) using sophisticated models. A new model (SnowModel) was recently developed for sea ice applications by colleagues at Colorado State University, and is now providing daily snow depth and density estimates from 1980 onwards. A key challenge is that different atmospheric reanalyses, which are used as input to the model, depict different amounts of precipitation. However, regardless of which reanalysis is used, from newer systems such as the NASA Modern-Era Retrospective analysis for Research and Applications-2 (MERRA-2) to older systems, such as the European Centre for Medium-Range Weather Forecasts (ECMWF) ERA-Interim (ERA-I), the increasing open water season has reduced the amount of annual snow being accumulated on the sea ice (Figure 5a and 5b). However, there is a lot of spatial variability in trends. There are trends toward shallower April snow depth over the coastal seas and trends toward deeper snow  over the central Arctic Ocean. Snow on sea ice plays several important roles such as influencing rates of thermodynamic ice growth each winter, melt pond development in summer, and melt water input to the upper ocean. Snow on sea ice also has important biological consequences by changing the amount of sunlight able to penetrate the ice.

Antarctic autumn—slow rise

As noted in last month’s post, Antarctica’s annual minimum extent occurred on March 1, the seventh lowest in the satellite record. Since the minimum, ice extent has increased at a slower-than-average pace, remaining well below the inter-decile (10 to 90 percent) range of past early autumn extents. Sea ice growth during March 2019 has been greatest in the central Ross Sea and northeastern Weddell Seas, with significant ice retreat continuing in the southern Bellingshausen Sea. In keeping with the relatively slow ice growth, air temperatures at the 925 mb level have been 2 to 4 degrees Celsius (4 to 7 degrees Fahrenheit) above the 1981 to 2010 average along much of the Antarctica coast from Wilkes Land eastward to the Ross, Amundsen, Bellingshausen, and Peninsula regions. Temperatures along the Dronning Maud Land coast have been 1 to 2 degrees Celsius (2 to 4 degrees Fahrenheit) below average. The atmospheric circulation at sea level has been characterized by three regions of higher than average pressure interspersed with areas of lower than average pressure, termed a wave-3 pattern by climate scientists. In particular, low pressure in the Amundsen Sea area and high pressure in the Drake Passage (between South American and the Antarctic Peninsula) produced strong winds from the northwest along the southern Peninsula, driving sea ice retreat there while other regions generally saw growth in sea ice extent.

Further reading

Stroeve, J., G. E. Liston, S. Buzzard, A. Barrett, M. Tschudi, M. Tsamados and J. S. Stewart. 2019. A lagrangian snow-evolution system for sea ice applications. Journal Geophysical Research-Oceans, submitted.

Liston, G. E., C. Polashenski, A. Roesel, P. Itkin, J. King, I. Merkouriadi and J. Haapala. 2018. A distributed snow-evolution model for sea-ice applications (SnowModel). Journal Geophysical Research-Oceans. doi.org/10.1002/2017JC013706.

Categories: Climate Science News

[SSALTO/DUACS] Jason-3 back in the NRT system as the reference mission

AVISO Climate Change News - Wed, 2019-03-27 03:25
A few weeks ago, the Jason-3 acquisition was stopped due to a safe-hold mode (SHM) event. The event itself was processed swiftly by the operations teams, and the ongoing Cal/Val investigations now report nominal quality metrics and no significant impact beyond the short interruption itself.   Because Jason-3 is the so-called reference altimeter in the multi-mission system DUACS (CMEMS Sea-Level TAC), the temporary unavailability called for an emergency procedure in the NRT system. The procedure uses a temporary anchor altimeter (here: Sentinel-3A) to stabilize the NRT system until the reference altimeter is back in operations.   Because the anchor is not a reference altimeter, the system slowly drifts away from what would have been produced with the reference altimeter (particularly in NRT). Now that Jason-3 has collected enough measurements after the SHM event, the drift was estimated. As expected it is small thanks to the good quality of Sentinel-3A, but not zero.   The procedure to seamlessly (no offset) reduce the drift to zero and to switch back to Jason-3 as the reference altimeter will be executed over this week where the system will be in a nominal status (no bias in the system).   All efforts are made to make this transition invisible to the CMEMS & DUACS end-users.   Please feel free to report any suspicious finding you might have during this period.
Categories: Climate Science News

Arctic sea ice maximum ties for seventh lowest in satellite record

NSIDC Artic Sea Ice News - Wed, 2019-03-20 10:00

Arctic sea ice appears to have reached its annual maximum extent on March 13, tying with 2007 for seventh lowest in the 40-year satellite record. The 2019 maximum sea ice extent is the highest since 2014. NSIDC will post a detailed analysis of the 2018 to 2019 winter sea ice conditions in our regular monthly post in early April.

Overview of conditions  National Snow and Ice Data Center|High-resolution image

Figure 1. Arctic sea ice extent for March 13, 2019 was 14.78 million square kilometers (5.71 million square miles). The orange line shows the 1981 to 2010 average extent for that day. Sea Ice Index data. About the data

Credit: National Snow and Ice Data Center
High-resolution image

On March 13, 2019, Arctic sea ice likely reached its maximum extent for the year, at 14.78 million square kilometers (5.71 million square miles), the seventh lowest in the 40-year satellite record, tying with 2007. This year’s maximum extent is 860,000 square kilometers (332,000 square miles) below the 1981 to 2010 average maximum of 15.64 million square kilometers (6.04 million square miles) and 370,000 square kilometers (143,000 square miles) above the lowest maximum of 14.41 million square kilometers (5.56 million square miles) set on March 7, 2017. Prior to 2019, the four lowest maximum extents occurred from 2015 to 2018.

The date of the maximum this year, March 13, was very close to the 1981 to 2010 median date of March 12.

Table 1. Ten lowest maximum Arctic sea ice extents (satellite record, 1979 to present) Rank Year In millions of square kilometers In millions of square miles Date 1 2017 14.41 5.56 March 7 2 2018 14.48 5.59 March 17 3 2016
2015 14.51
14.52 5.60
5.61 March 23
February 25 5 2011
2006 14.67
14.68 5.66
5.67 March 9
March 12 7 2007
2019 14.77
14.78 5.70
5.71 March 12
March 13 9 2005
2014 14.95
14.96 5.77
5.78 March 12
March 21

A recent paper (Meier and Stewart, 2019) describes the level of accuracy in NSIDC ice extent estimates, with the aim of improving annual minimum and maximum ranking of extents and to determine which years are close enough to be considered tied. For the Arctic maximum, which typically occurs in March, the uncertainty range is ~34,000 square kilometers (13,000 square miles), meaning that extents within this range must be considered effectively equal. The 2019 maximum extent is only 10,000 square kilometers (3,900 square miles) higher than the 2007 maximum, which is within this uncertainty range. Thus, we designate the 2007 and 2019 maximum extents as equal. As is shown in Table 1, other years have also been ascribed tied rankings. NSIDC scientists will rank future maximums and minimums using these criteria.

Final analysis pending

Please note this is a preliminary announcement of the sea ice maximum. At the beginning of April, NSIDC scientists will release a full analysis of winter conditions in the Arctic, along with monthly data for March. For more information about the maximum extent and what it means, see the NSIDC Icelights post, the Arctic sea ice maximum.

Further reading

Meier, W. N., and J. S. Stewart. 2019. Assessing uncertainties in sea ice extent climate indicators. Environmental Research Letters, 14, 035005. doi:10.1088/1748-9326/aaf52c.

 

Categories: Climate Science News

Planned outage on Extraction service and TDS Saturday March 16th

AVISO Climate Change News - Thu, 2019-03-14 02:58
Due to a planned outage, AVISO Extraction service and TDS (Opendap) are going to be unavailalble Saturday March 16th between 8h UTC and 15h UTC.
Categories: Climate Science News

Wind/Wave gridded products production recovery

AVISO Climate Change News - Wed, 2019-03-13 03:45
There were problems on the 3 satellites used to compute wind/wave maps : Jason-3 in Safe Hold Mode, Jason-2 also and Saral/AltiKa with strong problems. All this leaded to a stop in the processing of those products. Since  March 11th, there are some maps which are produced but they only content OGDR data of Jason-3. As from March 12th, IGDR data of Jason-3 will be introduced. Jason-2 and Saral have still some problems, so the date to reintroduce them it is not planned yet. 
Categories: Climate Science News

[Jason-3] Jason-3 instruments have been restarted successfully

AVISO Climate Change News - Thu, 2019-03-07 04:04
Jason-3 instruments have been restarted successfully on Wednesday, March, 6th, in cycle 113, pass 62 :
  • POSEIDON at 08:40:40UTC
  • AMR at 08:42:10UTC
  • GPSPB at 08:43:20UTC.
  The first telemetry from the satellite was available around 11UTC : OGDRs are now generated normally.
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March 2019: Focusing on small water bodies

AVISO Climate Change News - Wed, 2019-03-06 04:22
SAR-altimetry mode implemented onboard Sentinel-3 can be further refined so as to reach 50 cm...
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Ho hum February it may be, unless we speak of the Bering Sea

NSIDC Artic Sea Ice News - Mon, 2019-03-04 09:30

Arctic sea ice extent for February 2019 was the seventh lowest in the satellite record for the month, tying with 2015. So far this winter, sea ice extent has remained above the 2017 record low maximum. Extent in the northern Barents Sea, which has been quite low in recent years from “Atlantification,” is closer to average this February. Extent is very low in the Bering Sea at the end of February after unusual ice loss throughout the month. In Antarctica, the sea ice minimum may have been reached on both February 28 and March 1.

Overview of conditions  National Snow and Ice Data Center|High-resolution image

Figure 1a. Arctic sea ice extent for February 2019 was 14.40 million square kilometers (5.56 million square miles). The magenta line shows the 1981 to 2010 average extent for that month. Sea Ice Index data. About the data

Credit: National Snow and Ice Data Center
High-resolution image

Arctic sea ice extent for February 2019 averaged 14.40 million square kilometers (5.56 million square miles). This was 900,000 square kilometers (347,000 square miles) below the 1981 to 2010 long-term average extent, and 450,000 square kilometers (174,000 square miles) above the record low for the month set in February 2018. For the Arctic as a whole, February 2019 tied with 2015 for the seventh lowest average February extent in the 1979 to 2019 satellite record.

The daily average ice growth rate of 19,400 square kilometers (7,500 square miles) was near the long term average of 20,200 square kilometers (7,800 square miles). Ice growth during February primarily occurred in the Barents Sea and in the Sea of Okhotsk. Some ice growth was also observed in the Labrador Sea. Recent years have seen reduced ice coverage in the northern Barents Sea related to “Atlantification”—a greater influence of warm waters brought in from the Atlantic (see previous post). Sea ice extent toward the end of February 2019, however, was much closer to average in this region. By sharp contrast, sea ice extent drastically retreated in the Bering Sea in February and continues to as of this post.

Conditions in context

Figure 2a. The graph above shows Arctic sea ice extent as of March 4, 2019, along with daily ice extent data for four previous years and the record low year. 2018 to 2019 is shown in blue, 2017 to 2018 in green, 2016 to 2017 in orange, 2015 to 2016 in brown, 2014 to 2015 in purple, and 2011 to 2012 in dotted brown. The 1981 to 2010 median is in dark gray. The gray areas around the median line show the interquartile and interdecile ranges of the data. Sea Ice Index data.

Credit: National Snow and Ice Data Center
High-resolution image

 NSIDC courtesy NOAA Earth System Research Laboratory Physical Sciences Division| High-resolution image

Figure 2b. This plot shows the departure from average air temperature in the Arctic at the 925 hPa level, in degrees Celsius, for February 2019. Yellows and reds indicate higher than average temperatures; blues and purples indicate lower than average temperatures.

Credit: NSIDC courtesy NOAA Earth System Research Laboratory Physical Sciences Division
High-resolution image

Arctic temperatures at the 925 hPa level (approximately 2500 feet above the surface) were from 4 to 10 degrees Celsius (7 to 18 degrees Fahrenheit) above the 1981 to 2010 average for a region extending from the Bering Sea, through the Beaufort Sea, and into the Canadian Arctic Archipelago (Figure 2b). This is consistent with a pattern for the month of low pressure at sea level centered over the western Bering Sea, and high pressure centered over northwestern Canada (Figure 4b). Low pressure dominated both the central Arctic Ocean and the northern North Atlantic. As such, it comes as no surprise that the Arctic Oscillation index was positive overall for the month.

February 2019 compared to previous years February sea ice extent graph

Figure 3. Monthly February ice extent for 1979 to 2019 shows a decline of 3.0 percent per decade.

Credit: National Snow and Ice Data Center
High-resolution image

Overall, sea ice extent during February 2019 increased by 543,000 square kilometers (210,000 square miles). This was fairly close to the 1981 to 2010 average increase for the month. The linear rate of sea ice decline for February is 46,300 square kilometers (17,900 square miles) per year, or 3.0 percent per decade relative to the 1981 to 2010 average.

Ice loss in the Bering Sea This graph shows the sharp decline in sea ice extent in the Bering Sea starting at the end of January and continuing as of this post. The comparison map in the top left shows the difference is sea ice extent

Figure 4a. This graph shows the sharp decline in sea ice extent in the Bering Sea starting at the end of January and continuing as of this post. The inset map in the top left compares sea ice extent at the beginning of January 27 and at the end of March 3, 2019.

Credit: W. Meier, National Snow and Ice Data Center
High-resolution image

 NSIDC courtesy NOAA Earth System Research Laboratory Physical Sciences Division| High-resolution image

Figure 4b. This plot shows average sea level pressure in the Arctic in millibars (or hPa) for February 2019. Yellows and reds indicate high air pressure; blues and purples indicate low air pressure.

Credit: NSIDC courtesy NOAA Earth System Research Laboratory Physical Sciences Division
High-resolution image

As noted above, sea ice in the Bering Sea region is the most remarkable Arctic feature this month. On average, Bering sea ice extent increases until late March or early April. The ice in the region is volatile, responding to winds and waves. Extent often fluctuates during the winter when thin ice near the edge moves north or south and melts or grows. However, this year is quite extreme. From January 27 through March 3, extent decreased from 566,000 square kilometers (219,000 square miles) to 193,000 square kilometers (74,500 square miles), roughly equivalent to the size of Montana (Figure 4). A similar ice loss occurred last year, but 2018 and 2019 appear to be extreme in the satellite record. As of the beginning of March, the 2019 Bering Sea ice extent was the lowest in the satellite record for this time of year.

A major cause of the ice loss is the strong low pressure in the Bering Sea and the high pressure over northwestern Canada (Figure 4b). Strong winds between these pressure centers drew warm air into the region from the south, inhibiting ice growth in the Bering Sea while also pushing ice to the north. Storms also broke up large areas of ice near the ice edge and reduced the sea ice extent. Warmer than average sea surface temperatures have also been observed in the region.

An early look at sea ice freeboard from ICESat-2  R. Kwok, Jet Propulsion Laboratory|High-resolution image

Figure 5. These maps show preliminary sea ice freeboard (height of snow or ice surface above the ocean) from two weeks of ICESat-2 data acquired in October 2018. Note that both the spatial scale and the vertical scale are different for the two maps.

Credit: R. Kwok, Jet Propulsion Laboratory
High-resolution image

Colleague Ron Kwok of the Jet Propulsion Laboratory in Pasadena, CA, provided a first look of Arctic sea ice freeboard from the NASA Ice, Cloud and land Elevation Satellite 2 (ICESat-2) at the Fall 2018 American Geophysical Union conference. Freeboard represents the height of the top of the ice or snow above the adjacent ocean surface. Figure 5 shows the maps produced for both the Arctic and the Antarctic from the first two weeks of preliminary data from the satellite, October 14 to 28, 2018.

Freeboard measurements can be used to estimate sea ice thickness and volume, given certain assumptions. While in general freeboard and ice thickness increase and decrease together, the exact conversion from one to the other depends very much on snow thickness, snow and ice density, and degree of surface melt (if any). These maps are based on ~210 orbits using a single laser track from one of the six ICESat-2 laser profiles, smoothed to a 25-kilometer (15.5-mile) running average of the difference between snow and sea ice cover height, and ocean surface height. The ocean surface height is measured in ice-free ocean areas in gaps, or leads, within the sea ice.

Note how for the Arctic ICESat-2 captures the expected pattern of higher freeboard (thicker ice) north of the coast of the Canadian Arctic Archipelago and Greenland and lower freeboard (thinner ice) on the Eurasian side of the Arctic. As also expected, there is little thick ice (i.e. few areas with high freeboard) in Antarctica which consists of mostly first-year ice (less than 1 year old); the obvious exceptions are the areas of high freeboard in the northwestern Weddell Sea and along the northern coast of West Antarctica (Bellingshausen and Amundsen seas) where some older sea ice persists.

ICESat-2 data will be distributed by the NASA Snow and Ice Distributed Active Archive Center (DAAC) at NSIDC and will be available to the public soon.

Antarctic minimum sea ice extent was likely reached on February 28 and March 1

After plummeting in late December to record daily lows in sea ice extent, Antarctica’s melt slowed significantly in January and February, reaching its likely minimum of 2.47 million square kilometers (954,000 square miles) on both February 28 and March 1. This is the seventh lowest extent in the satellite record.

Sea ice extent has been particularly low in the central and eastern Weddell Sea and in the eastern Ross Sea, but above average ice extent remains along the East Antarctic coastline and the Bellingshausen Sea. Temperatures in the sea ice areas surrounding Antarctica have been near average to slightly below average at 1 degree Celsius to -2 degrees Celsius (34 degrees Fahrenheit to 28 degrees Fahrenheit), except in the Central Pacific/Ross Sea region where temperatures have been up to 3 degrees Celsius (5 degrees Fahrenheit) above the 1981 to 2010 average.

Further reading

Anchorage Daily: “Bering Sea ice is at an ‘unprecedented’ low right now”

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