Arctic News

Thursday, February 1, 2018

North Pole forecast to be above freezing on Feb 5, 2018

The image below shows a forecast of above freezing temperatures over the North Pole on Feb 5, 2018.

Above image shows a forecast of air temperature of 0.2°C or 32.4°F at 1000 hPa over the North Pole on February 5, 2018, 21:00 UTC.

Above image shows a forecast of temperatures of 1.1 °C or 33.9°F at the North Pole at 1000 hPa, on February 5, 2018, 18:00 UTC.

Above image shows a large area around the North Pole forecast to be up to 30°C or 54°F warmer than 1979-2000 on February 5, 2018.

Above image shows sea surface temperatures as high as 15.1°C or 59.2°F near Svalbard on February 9, 2018, in the panel on the left, and air temperatures as high as 6°C or 42.7°F (at 1000 hPa) near Svalbard on February 10, 2018, in the panel on the right.

These high temperatures are caused not only by ocean heat, but also by strong winds pushing warm air and water up from the North Atlantic into the Arctic. Above image shows the Jet Stream moving at speeds as high as 315 km/h or 196 mph (green circle, February 6, 2018, 6:00 UTC), moving in backward direction over Scandinavia, while extending over Antarctica and crossing the Equator at a number of places.

The decreasing temperature difference between the North Pole and the Equator is slowing down the speed at which the jet stream circumnavigates Earth and this is also making the jet stream more wavy.

As a more wavy jet stream extends deeper down over land, it allows cold air from the Arctic to flow down over land. As temperatures over land fall, the difference between ocean temperature and land temperature increases, especially in winter when land temperatures are much lower than ocean temperatures. This increasing difference between land and ocean temperature makes winds stronger and faster over oceans.

[ click on images to enlarge ]

In above image, the left panel shows a wavy jet stream speeding up over the North Atlantic, reaching speeds as high as 345 km/h or 215 mph (at green circle, 250 hPa).

In above image, the right panel shows strong winds pushing warm air from the Pacific Ocean through Bering Strait, resulting in temperatures over Alaska as high as 6.6°C or 44°F (at green circle, at 850 hPa).

The image on the right shows that waves as high as 8.27 m or 27.2 ft (at green circle) are forecast to enter the Arctic Ocean near Svalbard on February 5, 2018, giving an indication of the huge amount of energy that is going into oceans.

Earth is retaining more heat. This translates into higher surface temperatures, more heat getting stored in oceans and stronger winds. This in turn is causing higher waves and more evaporation from the sea surface. The image on the right shows a forecast of total amount of cloud water (in air from surface to space) of 1.5 kg/m² (green circle) in between Svalbard and the North Pole on February 5, 2018.

Warm air, warm water and high waves make it hard for sea ice to form, while evaporation from the ocean adds more water vapor to the atmosphere. Since water vapor is a potent greenhouse gas, this further accelerates warming of the Arctic.

The high temperatures at the North Pole follow high temperatures over East Siberia, as illustrated by the image below.

Above image shows average temperature anomalies for January 31, 2018, compared to 1979-2000. The image below shows open water on the East Siberian coast in the Arctic Ocean that day.

Meanwhile, Arctic sea ice extent is very low. The image below shows that extent on January 30, 2018, was 13.391 million km², a record low for the time of the year.

In the video below, Paul Beckwith discusses the situation.

In the podcast below, by Wolfgang Werminghausen, entitled Sam Carana about the Arctic and global temperature, Sam Carana's responses are read by Kevin Hester.

From the interview, Sam Carana: "Methane releases from the seafloor of the Arctic Ocean have a strong warming impact, especially locally, AND methane releases in the Arctic also act as a catalyst for other feedbacks that are all self-reinforcing and interlinked, amplifying each other in many ways. It could easily become 10°C or 18°F warmer in a matter of years, especially in places where most people are now living."

The image below shows that on February 11, 2018, methane reached peak levels as high as 2925 ppb.

High methane peaks are becoming more common as the water temperature of oceans keeps rising, which also goes hand in hand with more water vapor and less sea ice. As said, these are all warming elements that amplify each other in many ways.

On Feb 8, 2018, Antarctic sea ice extent was 2.382 million km², a record low for the time of the year and 1.811 million km² less than the extent on Feb 8, 2014.

The image on the right illustrates the huge loss of sea ice around Antarctica over the past few years. Antarctic sea ice looks set to reach an all-time low extent later this month, with a difference of close to 2 million km² persisting, compared to just a few years ago.

The image below shows a forecast for February 5, 2018, with as much as 3.84 kg/m² (green circle) Total Cloud Water in between South Africa and Antarctica.

More water vapor in the air contributes to global warming, since water vapor is a potent greenhouse gas. The image below shows a forecast for February 5, 2018, with temperatures on Antarctica reaching as high as 8.9°C or 47.9°F (update Feb. 11, 2018: 7.1°C or 44.7°F at 78°S, 17°E at 1000 hPa on Feb. 5, 2018, 15:00z).

At this time of year, global sea ice is typically at its lowest extent for the year. On February 9, 2018, global sea ice reached the lowest extent on record, as illustrated by the image below by Wipneus.

This means that a huge amount of sunlight that was previously reflected back into space is now instead getting absorbed by oceans.

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

Monday, January 22, 2018

2017 was hottest year on record

The year 2017 was the hottest year on record, as the image below illustrates.

When determining which year was the hottest year, care should be taken to avoid bias due to temporary conditions such as the El Niño that was present in 2016 and the La Niña we're now experiencing now. Above image uses NASA land+ocean January 2012-December 2017 anomalies from 1951-1980, adjusted by 0.59°C to cater for the rise from preindustrial to 1951-1980, to calculate a linear trend that goes some way to smooth out variability due to El Niño/La Niña events. The trend shows that 2017 was significantly warmer than 2016.

The trend also shows that 1.5°C above preindustrial was crossed back in 2016. This 1.5°C (or 2.7°F) was set at the Paris Agreement as a guardrail that was not to be crossed. The trend further shows that we've meanwhile crossed 1.6°C above preindustrial and we look set to cross the 2°C guardrail within years.

Global warming has crossed 1.5°C / 2.7°F above preindustrial and looks set to cross 2°C / 3.6°F soon. Due to accelerating warming in the Arctic, that could happen within one or two years time, i.e. much faster than the trendlines below may suggest.

Indeed, warming in the Arctic is taking place much faster than elsewhere, and the difference is accelerating. There's a huge danger that accelerating warming in the Arctic will speed up feedbacks such as:
• huge amounts of methane getting released from the seafloor of the Arctic Ocean;
• melting of sea ice and permafrost causing more sunlight to get absorbed in the Arctic, as less sunlight gets reflected back into space;
• changes to jet streams causing more extreme weather, in turn resulting in more emissions, such as due to wildfires;
• and more.

In conclusion, feedbacks could speed up global warming by much more than what may be suggested by above trends that look only at surface temperature of the atmosphere and that are based on previous data when such feedbacks had yet to become manifest.

Add up the impact of all warming elements and, as an earlier analysis shows, the rise in mean global temperatures from preindustrial could be more than 10°C in a matter of years, as illustrated by the image below, which shows a much steeper rise.

Particularly devastating feedbacks could result from changes regarding heat and carbon dioxide taken up by oceans. Oceans now take up 93.4% of global warming, as illustrated by the image below.

As said, when looking at surface temperatures of the atmosphere, there will be bias due to El Niño/La Niña events. One way to smooth out such bias is by calculating trendlines over many years. Another way to compensate for such bias is to also look at ocean heat. In terms of ocean heat, the year 2017 stands at the top, as the left panel of above image illustrates. In 2016, El Niño caused relatively more heat to be present in the atmosphere and less in oceans, whereas the opposite occurred in 2017, contributing to the fact that in 2017 a record amount of ocean heat was recorded. Occurrence of El Niño/La Niña events over the years is visualized by the image below.

One danger is that, in future, there will be more impact by El Niño events and less by La Niña events. A recent study concludes that as temperatures rise due to emissions by people, the frequency, magnitude and duration of strong El Niño events will increase.

In addition to higher temperature peaks due to El Niño events, more heat could remain in the atmosphere as the rise in temperature in general causes greater ocean stratification, making that less heat gets absorbed by oceans, as discussed in several earlier posts. The image below depicts this feedback and further feedbacks mentioned above. Feedbacks are described in more detail at the feedbacks page.

The situation is further illustrated by the danger assessment below.

[ Danger Assessment, from earlier post ]

Meanwhile, the Global Carbon Project projects a growth of 2% for the 2017 global carbon dioxide emissions from fossil fuels and industry (including cement production), compared to 2016 levels, as illustrated by image below.

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 ]

Sunday, December 24, 2017

Winds keep changing as warming continues

November 2017 was 0.87 degrees Celsius warmer than the mean 1951-1980 November temperature, as above image shows. The last three Novembers — 2015, 2016, and 2017 — are the three warmest in the entire modern record. The warmest month of November happened in 2015 (+1.03°C) when there was a strong El Niño, while we're currently in a La Niña period.

On the image below, cyclonic winds on December 21, 2017, are visible near the Philippines and Vietnam. Near the Philippines, 3-hour precipitation accumulation was as high as 121.6 mm or 4.79 in (at green circle). As a BBC report describes, Tropical Storm Tembin made landfall in the southern Philippines on December 22, 2017, causing flash flooding and mudslides. More than 180 people are reported to have been killed, as the tropical storm swept through Mindanao island, with dozens more missing.

A week earlier, Tropical Storm Kai-Tak hit the central Philippines, killing dozens. The region is still recovering from Typhoon Haiyan, which killed more than 5,000 people and affected millions in 2013.

The winds are fueled by high sea surface temperatures. Above image shows that, on December 21, 2017, sea surface temperatures were as high as 31.7°C or 89°F north of Australia. In line with rising temperatures caused by global warming, sea surface temperature anomalies are high across the oceans, as the image below illustrates.

As above image also shows, the sea surface was relatively cold at locations indicative for El Niño (depicted as four El Niño regions on the right).

The image below shows El Niño forecast plumes indicating that we're currently in a La Niña period, and that temperatures are on the rise.

In conclusion, just like the rise in temperatures is currently masked by a La Niña period, the return to a new El Niño period will further strengthen the rise.

This strengthening of winds is what can be expected in a warmer world. Above image shows a wavy Northern Polar Jet Stream combine with the Northern Subtropical Jet Stream to reach speeds as high as 401 km/h or 249 mph.

As the jet stream becomes more wavy and extends over the Arctic, more warm air and water gets carried into the Arctic, further speeding up warming, as also discussed at The Arctic is changing the Jet Stream - Why This Is Important.

The importance of Arctic warming was also discussed in the recent post Warming is accelerating. Changes to the Jet Stream can cause a lot more heat to be brought into the Arctic, through both the Bering Strait and the Fram Strait. This image below shows wind through the Bering Strait reaching speeds as high as 135 km/h or 84 mph.

The combination image below shows the Jet Stream extending over the Arctic Ocean and remaining in place for days, reaching speeds as high as 206 km/h or 128 mph. Such 'blocking' patterns can cause a lot of heat to be brought into the Arctic atmosphere, as well as into the water of the Arctic Ocean. The image in the left-hand panel indicates that temperature anomalies over the Arctic Ocean could be as high as 30°C or 54°F.

[ click on images to enlarge ]

As the temperature difference between the North Pole and the Equator decreases, the Jet Stream becomes more wavy, at times extending deep over the continents and bringing cold air to the south. This further increases the (already high) temperature difference between land and ocean, further speeding up cyclonic winds that move over the oceans toward the North Pole and that carry warm water and air toward the Arctic Ocean. The image below shows a forecast for January 1, 2018.

As sea ice keeps declining, ever less sunlight gets reflected back into space. The image below shows the decline in global sea ice area over the years.

The image below shows the average year-to-date Arctic sea ice volume (PIOMAS data).

This further confirms the updated trend analysis of the NASA temperature anomaly below.