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    Showing posts with label hydrates. Show all posts
    Showing posts with label hydrates. Show all posts

    Tuesday, January 2, 2018

    Unfolding Arctic Catastrophe

    On January 1, 2018, methane levels as high as 2764 ppb (parts per billion) were recorded. The solid magenta-colored areas near Greenland indicate that this very high reading was likely caused by methane hydrate destabilization in the sediments on the seafloor of the Arctic Ocean.


    The state of the sea ice is behind this. On January 1, 2018, Arctic sea ice extent was at record low for the time of the year. The smaller the extent, the less sunlight gets reflected back into space and is instead absorbed in the Arctic.

    At this time of year, though, hardly any sunshine is reaching the Arctic. So, what triggered this destabilization? As the image below indicates, year-to-date average Arctic sea ice volume has been at record low in 2017, which means that there has been very little sea ice underneath the surface throughout 2017.


    Warm water will melt the sea ice from below, which keeps the water at greater depth cool. However, when there is little or no sea ice underneath the surface, little or no heat will be absorbed by the process of melting and the heat instead stays in the water, with the danger that it will reach sediments at the bottom of the Arctic Ocean, as illustrated by the image below.

    The Buffer has gone, feedback #14 on the Feedbacks page
    [ image from: Warming is accelerating ]
    The image on the right shows warm water from the North Atlantic arriving near Svalbard. How warm is the water beneath the surface of the Arctic Ocean? The image below gives an indication, showing how much warmer the water was from October 1, 2017, to December 30, 2017, at selected areas near Svalbard, where warm water from the North Atlantic dives under the sea ice of the Arctic Ocean, carried by the Gulf Stream.

    [ click on images to enlarge ]
    In 1981-2011, temperatures were gradually falling by more than one degree Celsius from October 1 to the December 21 Solstice, then started to rise again in line with the change in seasons (blue line). In 2017, temperatures were rising in October. On October 25, 2017, the sea surface was as warm as 17.5°C or 63.5°F, i.e. a 14.1°C or 24.5°F anomaly. On average, it was 12.96°C or 23.35°F warmer during the period from October 1 to December 30, 2017 (red line), compared to the same days in 1981-2011.

    The images below further illustrate the situation. Surface temperature of the atmosphere near Svalbard was as warm as 7°C or 44.5°F on January 13, 2018 (at green circle, left panel). The sea surface near Svalbard was as warm as 15.9°C or 60.8°F on January 12, 2018, compared to 2.4°C or 36.4°F on January 12 for the period 1981-2011 (at green circle, center panel). Waves as high as 13.04 m or 42.8 ft (at green circle, right panel) batter the North Atlantic along Norway's coast all the way to Svalbard on January 15, 2018.


    The image below shows that waves as high as 16.01 m or 52.5 ft are forecast to batter the North Atlantic on January 16, 2018 (green circle, left panel). 100% relative humidity is recorded over the Arctic Ocean on January 15, 2018 (green circle, center panel). The Jet Stream reaches speeds as high as 426 km/h or 264 mph on January 15, 2018 (green circle, right panel).


    Similar extreme weather patterns can be seen elsewhere in the Arctic. The image below on the left shows that temperatures as high as 18.5°C or 65.3°F were recorded on Jan. 14 and 15, 2018 in Metlakatla, Alaska. The image below on the right shows that surface temperatures as high as 7.4°C or 45.2°F were reached on January 16, 2018, in Yukon Territory, Canada (at green circle).

    [ click on images to enlarge ]

    In conclusion, as the Arctic is warming up faster than the rest of the world, Jet Streams are getting more wavy, resulting in more extreme weather events. Wind speed accelerates over warmer oceans, pushing more heat into the Arctic Ocean, threatening to cause eruptions of huge amounts of methane from the Arctic Ocean seafloor.

    The situation is dire and calls for comprehensive and effective action as described at the Climate Plan.


    Links

    • Climate Plan
    https://arctic-news.blogspot.com/p/climateplan.html

    • Warming is accelerating
    https://arctic-news.blogspot.com/2017/11/warming-is-accelerating.html

    • Feedbacks
    https://arctic-news.blogspot.com/p/feedbacks.html

    • 10°C or 18°F warmer by 2021?
    https://arctic-news.blogspot.com/2017/04/10c-or-18f-warmer-by-2021.html

    • Abrupt Warming - How Much And How Fast?
    https://arctic-news.blogspot.com/2017/05/abrupt-warming-how-much-and-how-fast.html

    • Accelerating growth in CO₂ levels in the atmosphere
    https://arctic-news.blogspot.com/2017/02/accelerating-growth-in-co2-levels-in-the-atmosphere.html

    • High methane levels over the Arctic Ocean on January 14, 2014
    https://arctic-news.blogspot.com/2014/01/high-methane-levels-over-the-arctic-ocean-on-january-14-2014.html

    • Extinction
    https://arctic-news.blogspot.com/p/extinction.html

    • Methane Erupting From Arctic Ocean Seafloor
    https://arctic-news.blogspot.com/2017/03/methane-erupting-from-arctic-ocean-seafloor.html

    • 2015 warmest year on record
    https://arctic-news.blogspot.com/2015/12/2015-warmest-year-on-record.html

    • Accelerating Warming of the Arctic Ocean
    https://arctic-news.blogspot.com/2016/12/accelerating-warming-of-the-arctic-ocean.html

    • Arctic Ocean Feedbacks
    https://arctic-news.blogspot.com/2017/01/arctic-ocean-feedbacks.html

    • Warning of mass extinction of species, including humans, within one decade
    https://arctic-news.blogspot.com/2017/02/warning-of-mass-extinction-of-species-including-humans-within-one-decade.html

    Wednesday, August 2, 2017

    Arctic sea ice may well be gone by September 2017

    The Arctic Ocean is warming up fast and this is melting the sea ice from below.

    Sea surface temperature anomalies are well above 8°C (14.4°F) in several parts of the Arctic Ocean.

    The image on the right shows sea surface temperature anomalies from 1961-1990 for the Arctic (60°N - 90°N) on August 2, 2017.

    Global sea ice extent is at a record low for the time of the year, as illustrated by the graph below, by Wipneus. Lower sea ice extent means that less sunlight is reflected back into space.


    Arctic sea ice extent in 2017 is shrinking along a path that currently looks similar to the years 2012, 2016 and 2007, when sea ice reached 1st, 2nd and 3rd place, respectively, regarding lowest extent (image right).

    Arctic sea ice volume has been at record low since the start of 2017 and is currently similar to 2012, as illustrated by the graph below right, by Wipneus (click on images to enlarge them).

    Arctic sea ice may look to be similar to what it was in 2012, when extent and volume reached lowest since satellite measurements began.

    However, sea ice thickness has fallen dramatically over the years in the areas where previously was the thickest ice.

    This is illustrated by the combination image below, showing Arctic sea ice thickness (in m) in July 31, 2012 (left panel) versus thickness on July 31, 2017 (right panel).

    [ click to enlarge ]
    The navy.mil animation on the right shows sea ice getting thinner recently, with especially the thicker sea ice disappearing fast.

    There appear to be discrepancies between the PIOMASS calculation of ice volume and the ice thickness images by navy.mil.
    This may be due to the way volume is calculated and may be similar to differences in extent and area.

    Sea ice clearly has disappeared most where once the thickest ice was present.


    Harold Hensel points out that extent may at first glance show more ice but each cell in a grid may only have 15% of ice present to be labeled 'ice-covered'. Harold adds an image showing ice concentration, which gives another insight in the shape and condition of the sea ice (above image).

    Paul Beckwith and Patrick McNulty bluntly conclude that PIOMAS is wrong, as illustrated by the Twitter screenshot on the right.

    Clearly, dramatic shrinking of the thicker sea ice has occurred over the past few years and one of the reasons for this is the ever warmer water that is getting pushed into the Arctic Ocean along the Gulf Stream. This is melting the sea ice from below. Warming of the Arctic Ocean heats up the air over the Arctic Ocean, as illustrated by the image below.


    [ click on image to enlarge ]
    The above image shows a 365-day surface temperature anomaly. The change over time is also illustrated by the animation on the right.

    On average, surface temperatures over the Arctic Ocean have been more than 2.5°C (or 4.5°F) warmer than in 1981-2010. The warmer air is now also melting the sea ice from above, as temperatures over the Arctic have risen to well above the freezing point.

    High temperatures over the Arctic Ocean means that precipitation no longer takes the form of snow, but instead falls in the form of rain.


    Below is a further warning, against a more recent background image (situation on August 6, 2017).


    [ click on image to enlarge ]
    High temperatures of the surface of the ocean combined with strong winds makes that a lot of moisture is rising from the sea surface to the atmosphere.

    The image on the right shows that sea surface temperatures in the Bering Strait were as high as 19°C (or 66.2°F) on July 22, 2017. This is partly the result of warm water from rivers entering the Bering Strait.

    Furthermore, cyclones can make winds reach high speeds, as illustrated by the image below, showing Typhoon Noru approaching Japan.

    The image shows a forecast for August 5, 2017, 18:00 UTC. Waves have been forecast to be as high as 16.15 m or 53 ft, while winds have been forecast to be as fast as 214 km/h or 133 mph or 116 kn.

    [ click on image to enlarge ]
    Total precipitable water has been forecast to be as much as 91.000 kg/m² and 3-hr Precipitation Accumulation has been forecast to be as much as 281.3 mm (or 281.3 kg/m²) or 11.07 in.

    Back to the Arctic, where strong winds and moist air combine to make a lot of rain, as temperatures are well above freezing in most areas, as illustrated by the image on the right (showing air temperature at 2 m).

    The image below shows how strong winds are pushing warm and moist air through the Bering Strait on July 31, 2017 at surface level (left), at 700 hPa (center) and at 250 hPa (right), where the jet stream used to separate the cold air in the Arctic from the warmer air further south.


    As above image also shows, the jet stream is getting more and more out of shape, at places crossing the Arctic Ocean. In the video below, Paul Beckwith discusses the situation in the Arctic.


    The image below shows trends for both Arctic and Antarctic sea ice area pointing downward.


    When looking at sea ice volume, zero sea ice in September 2017 is within the margins of the trendline below on the right.

    [ Arctic sea ice, gone by Sept. 2017? ]
    Given the speed at which many feedbacks can kick in and the interaction between warming elements, Arctic sea ice volume may well be gone by September 2017.

    The low sea ice volume means that there is very little sea ice left to act as a buffer this year. Therefore, a huge amount of heat will not be able to be consumed this year in the process of melting ice and will instead speed up warming of water of the Arctic Ocean.

    Less sea ice additionally means that less sunlight will be reflected back into space, and this heat will instead further speed up Arctic warming.

    The Buffer has gone, feedback #14 on the Feedbacks page

    Where can all this extra heat go? Sea ice is expected to start sealing off much of the surface of the Arctic Ocean by the end of September 2017, which will make it harder for heat to escape the Arctic Ocean by entering the atmosphere.

    The danger is that much of the extra heat will instead reach sediments at the seafloor of the Arctic Ocean that contain huge amounts of methane in currently still frozen hydrates.

    The image on the right shows that methane reached levels as high as 2583 ppb on July 31, 2017.

    The image also shows high methane levels over Antarctica where hydrate destabilization also appears to be taking place, as discussed in an earlier post.

    The situation is dire and calls for comprehensive and effective action, as described at the Climate Plan.


    Links

    • Climate Plan
    https://arctic-news.blogspot.com/p/climateplan.html

    • 10°C or 18°F warmer by 2021?
    https://arctic-news.blogspot.com/2017/04/10c-or-18f-warmer-by-2021.html

    • Abrupt Warming - How Much And How Fast?
    https://arctic-news.blogspot.com/2017/05/abrupt-warming-how-much-and-how-fast.html

    • Accelerating growth in CO₂ levels in the atmosphere
    https://arctic-news.blogspot.com/2017/02/accelerating-growth-in-co2-levels-in-the-atmosphere.html

    • Feedbacks
    https://arctic-news.blogspot.com/p/feedbacks.html

    • Extinction
    https://arctic-news.blogspot.com/p/extinction.html

    • Methane Erupting From Arctic Ocean Seafloor
    https://arctic-news.blogspot.com/2017/03/methane-erupting-from-arctic-ocean-seafloor.html

    • Warning of mass extinction of species, including humans, within one decade
    https://arctic-news.blogspot.com/2017/02/warning-of-mass-extinction-of-species-including-humans-within-one-decade.html



    Sunday, May 14, 2017

    Earthquake east of Greenland triggers methane releases


    An earthquake with a magnitude of M 4.5 on the Richter scale hit the seafloor 204 km East of Nord, Greenland, on May 8, 2017 at 04:48:53 (UTC). Location: 81.684°N 5.076°W. Depth: 10.0 km.

    The inset shows that methane levels over 1950 ppb (magenta color) were recorded on the morning of May 8, 2017, by two satellites.

    This is a reminder that earthquakes can destabilize methane hydrates, which can hold huge amounts of methane in sediments at the seafloor of the Arctic Ocean. As temperatures keep rising, snow and ice on Greenland and Svalbard keeps melting, taking away weight from the surface, making that isostatic rebound can increasingly trigger earthquakes on the faultline that crosses the Arctic Ocean.

    Methane releases have followed earthquakes in the Arctic before, e.g. see this 2016 post, illustrating the danger of potentially huge methane releases in case of larger earthquakes in the Arctic.

    Why is methane so important again? Below follow some images from the methane page


    Over a 10-year timescale, methane emissions cause more warming than carbon dioxide emissions, as illustrated by the graph in the left-hand panel of above image.

    Methane levels fluctuate with the time of year, higher mean levels are typically reached in September.

    On September 14, 2016, methane levels at 367 mb were as high as 2697 ppb (locally), while global mean methane level was as high as 1865 ppb (above image).

    On May 13, 2017, am, global mean methane levels were as high as 1844 ppb at altitudes corresponding to 383mb to 469 mb (MetOp-1 satellite), while local levels as high as 2485 ppb were recorded.

    Methane levels have risen 256% from 1750 to 2015, as illustrated by the image on the right.

    Growth in methane levels has been accelerating recently. Contained in existing data is a trend indicating that methane levels could increase by a third by 2030 and could almost double by 2040, as illustrated by the image below. 


    The situation is dire and calls for comprehensive and effective action, as described at the Climate Plan.


    Links

    • Climate Plan
    https://arctic-news.blogspot.com/p/climateplan.html

    • High Methane Levels Follow Earthquake in Arctic Ocean
    https://arctic-news.blogspot.com/2016/07/high-methane-levels-follow-earthquake-in-arctic-ocean.html

    • Methane
    https://arctic-news.blogspot.com/p/methane.html


    Thursday, May 11, 2017

    Arctic Sea Ice May 2017

    Last year, the Arctic was some 3.5°C warmer than it was at the start of the Industrial Revolution. Was this 3.5°C a spike or was it part of a trend pointing at even higher temperature anomalies this year and the following years?


    Above image shows NASA annual mean 64°N-90°N land-ocean temperature anomalies from 1951-1980, with +0.59°C added for the rise from 1750 to 1951-1980. A polynomial trend is added (based on 1880-2016 data), pointing at 4.5°C anomaly by 2019.

    Will the Arctic keep warming over the coming years in line with this trend? Let's have a look at what affects temperatures in the Arctic most, specifically Ocean Heat, Sea Ice, Land Temperatures and Emissions.

    1. Ocean Heat

    Warmer Oceans on the Northern Hemisphere will contribute strongly to warming in the Arctic. Here's a graph showing a trend pointing at continued warming of the oceans on the Northern Hemisphere.

    Will oceans keep warming like that, in particular the North Atlantic? The Coriolis force keeps pushing warm water of the North Atlantic along the Gulf Stream toward the Arctic Ocean.

    On the image on the right, the Gulf Stream shows up as the warmer water (orange and yellow) off the coast of North America.

    Thus, as oceans keep warming, warmer water will reach the Arctic Ocean, melting the sea ice from below.

    The image on the right shows that the sea surface was 9.3°C or 16.8°F warmer than 1981-2011 on May 7, 2017, at the location marked by the green circle.

    2. Sea ice

    Meanwhile, the sun will warm up the sea ice from above. The sea ice acts as a barrier, insulating the water of the Arctic Ocean from the heat from above. As long as there is sea ice, water just underneath the sea ice will stay close to freezing point.

    Sea ice can strongly affect the amount of heat that is retained by Earth. Sea ice reflects most sunlight back into space, but in the absence of sea ice, most sunlight will instead be absorbed by oceans.

    For almost a year now, global sea ice extent has been way below what it used to be, meaning that huge amounts of sunlight that were previously reflected back into space, are now instead getting absorbed by Earth, as shown by the graph below (by Wipneus).

    Over the past 365 days, most of the Arctic has been more than 2.5°C or 4.5°F warmer than it was in 1981-2010, as the image on the right illustrates. Note also the anomalies around Antarctica. Decline of the snow and ice cover contributes strongly to these temperature anomalies.

    When looking at albedo changes, sea ice area is an even more critical measure than sea ice extent. For a discussion of the difference between area and extent, see this NSIDC page. The image below shows trends for both Arctic and Antarctic sea ice area pointing downward.


    When looking at sea ice volume, zero sea ice in September 2017 is within the margins of the trendline below on the right.

    [ Arctic sea ice, gone by Sept. 2017? ]
    Given the speed at which many feedbacks can kick in and the interaction between warming elements, Arctic sea ice volume could be zero by September 2017.

    Arctic sea ice is at a record low volume for the time of the year (see graph below by Wipneus). This means that there is very little sea ice left to act as a buffer this year. Therefore, heat that won't be consumed in the process of melting the ice will instead speed up Arctic warming.

    As said - less sea ice additionally makes that less sunlight will be reflected back into space, and that instead more heat will speed up Arctic warming.
    As the sea ice gets thinner, it becomes more fragile. Furthermore, changes to the Jet Stream can fuel strong winds and waves, which are also more likely to hit the ice as the size of the open water increases.

    The satellite image below of the Beaufort Sea shows that the sea ice is cracked in many places and broken into pieces by winds, waves, currents and ocean heat. A huge crack can be seen running along the Canadian Archipelago toward Greenland (bottom right on the image).


    An animation (1.3 MB) is added at the end of this post showing the sea ice breaking into pieces in the Beaufort Sea from April 26 to May 10, 2017. It illustrates that a combined force of winds, waves, currents and ocean heat can break even the thicker ice into pieces, with the danger that all ice can be pushed out of the Arctic Ocean.

    3. Temperatures on land

    High temperatures on land will affect the Arctic in a number of ways. What kind of temperatures can be expected over the coming months, which are so critical for Arctic sea ice?

    - Heatwaves

    Heatwaves over the continents can more easily extend over the Arctic Ocean as the Northern Polar Jet Stream becomes more wavy. Heatwave conditions are more likely to occur as the jet stream is changing due to accelerated warming of the Arctic.

    - Wildfires

    High temperatures on land can also cause wildfires that can in turn cause huge quantities of emissions, including soot that when settling on snow and ice, can strongly speed up melting. The image below shows carbon dioxide as high as 607 ppm and carbon monoxide as high as 24.84 over Laos on May 4, 2017.


    - Warm water from rivers flowing into the Arctic Ocean

    Furthermore, high temperatures on land will warm up the water of rivers flowing into the Arctic Ocean.

    - El Niño

    An El Niño event can dramatically boost temperatures of the atmosphere. What are the projections for an El Niño in 2017? The image on the right, by the ECMWF (European Centre for Medium-Range Weather Forecasts), indicates an El Niño that is gaining strength.

    4. Emissions and Greenhouse Gas Levels

    Continued emissions and high greenhouse gas levels are responsible for warming of the planet. Have efforts to cut emissions been successful? Is growth in greenhouse gas levels slowing down? The image below shows accelerating growth of carbon dioxide levels recorded at Mauna Loa, Hawaii.

    The image below shows carbon dioxide levels recorded at Barrow, Alaska.

    The image below shows methane levels at Barrow, Alaska.
    In conclusion, indications are that warming in the Arctic will continue in 2017, which spells bad news for Arctic sea ice and for the world at large, as discussed in earlier posts.

    The situation is dire and calls for comprehensive and effective action, as described in the Climate Plan.


    The animation below shows the break up of the sea ice in the Beaufort Sea from April 26 to May 10, 2017. It illustrates that a combined force of winds, waves, currents and ocean heat can break even the thicker ice into pieces, with the danger that all ice can be pushed out of the Arctic Ocean.


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