Sunday, August 18, 2013

Methane Jump



Methane Jump - a video created by Sam Carana with methanetracker.org for Arctic-news.blogspot.com



The video shows high methane levels during the period July 16 - August 16, 2013, as recorded by IASI, MetOp2 Satellite. The video shows how high levels can get, mentioning that methane readings suddenly jumped dramatically, with levels recorded as high as 2349 ppb (on August 1, 2013). Later in August 2013, methane reached even higher levels. The image below shows readings as high as 2442 ppb on August 5, 2013.


We can count ourselves lucky that - until now - only a small part of the methane appears to be released from the Arctic seabed, but such releases threaten to send huge quantities of methane into the atmosphere rather abruptly, triggering runaway global warming and ending civilization as we know it in a matter of decades.

Below a comparison of early August methane levels over the years, created from images by Leonid Yurganov.


Below are two maps with methane lvels at over 1950 ppb, for the Northern Hemisphere and the Southern Hemisphere, respectively, for the period from July 16 to August 24, 2013.



The chart below shows average values of methane for the same period, with a peak level of 1862 ppb on August 2, 2013, on the Northern Hemisphere.


As the above chart illustrates, the methane jump occurred early August, 2013, both on the Northern Hemisphere and on the Southern Hemisphere. Assuming a total burden of methane in the atmosphere of roughly 5 Gt at an average value of 1800 ppb, then a simple division results in an additional burden of 2.78 Mt for each rise of one ppb, implying that a methane jump of 20 ppb corresponds with an additional burden of about 56 Mt (or 56 billion kg) of methane in the atmosphere.


Related

- Arctic Ocean is turning red
http://arctic-news.blogspot.com/2013/08/arctic-ocean-is-turning-red.html

- Dramatic rise in methane levels since end July 2013
http://arctic-news.blogspot.com/2013/08/dramatic-rise-in-methane-levels-since-end-july-2013.html

- Methane levels remain very high around the globe
http://arctic-news.blogspot.com/2013/08/methane-levels-remain-very-high-around-the-globe.html

- Methane levels keep rising rapidly
http://arctic-news.blogspot.com/2013/08/methane-levels-keep-rising-rapidly.html

- Methane as high as 2349 ppb
http://arctic-news.blogspot.com/2013/08/methane-as-high-as-2349-ppb.html

- Where does the methane come from?
http://arctic-news.blogspot.com/2013/08/where-does-the-methane-come-from.html

- Conversion table (Gt and Mt to kg, etc.)
http://arcticmethane.blogspot.com/p/fact.html

Friday, August 16, 2013

Four Hiroshima bombs a second: how we imagine climate change

Hiroshima bomb - from: Wikipedia image
Where does the excess heat go that is trapped in our atmosphere by greenhouse gases every day?

The title of this post is a hat-tip to David Holmes, Monash University, Australia, who recently published an article with that title at The Conversation, discussing that the daily excess heat absorbed by Earth equals the heat released by well over four Hiroshima bombs every seconds.

It's actually well over four Hiroshima bombs every second, given that there are 86,400 seconds in a day and based on James Hansen calculations (at a Feb 29, 2013, TED presentation) that the current imbalance of 0.6 watts/square meter (which does not include the energy already used to cause the current warming of 0.8°C) was equivalent to exploding 400,000 Hiroshima atomic bombs every day, 365 days per year.

As illustrated by the graph below, most of this excess heat is absorbed by oceans and ice. Some of the heat is consumed by the process of melting ice into water, but most heat ends up warming up the oceans.
Graph by Sceptical Science
An earlier post (September 2012, added underneath) described the study by Nuccitelli et al. that measures heat going into the oceans in Joules and, as discussed above, measuring excess heat in terms of heat released by nuclear bombs might give more meaning to what is going on.

Where does the extra heat go? 

Global warming is causing Earth to heat up. As shown on the image below, by Nuccitelli et al., most heat goes into the oceans. A substantial amount of heat also goes into the melting of ice.





Warming of water in the Arctic Ocean

Global warming is heating up the oceans big time. As the image below shows, the global ocean heat content has been rising for many years.



White arrows mark ice drift directions. Red arrows mark 
the transport path of warm Atlantic water entering the 
Arctic where it submerges under the cold, ice-covered 
surface layer. Robert Spielhagen (IFM-GEOMAR, Kiel)
The Arctic is affected in particular by the Thermohaline Circulation.

Water flowing into the Arctic Ocean from the Atlantic Ocean is about 2°C warmer today than it has been for at least 2,000 years, according to a study published in Science. The current of warm water lies 50 metres below the surface, and can reach 6°C in summer — warm compared to Arctic surface waters, which can be -2°C.

At the same time, cold water and sea ice are driven out of the Arctic Ocean, along the edges of Greenland. The net result is a marked increase in the temperature of the water in the Arctic Ocean, especially the top layer of the water which causes the sea ice to melt.

The Arctic radiates comparatively less heat into space

Furthermore, cold layers of air close to the surface of the Arctic Ocean make it difficult for infrared radiation to go out to space, according to a study published in Science. These layers do warm up, but warming of these layers is directed downwards, thus amplifying warming in the Arctic.

Surface air temperatures in the Arctic are rising rapidly

Anomalies for surface air temperatures are higher in the Arctic than anywhere else on Earth. The increase in temperature anomalies appears to be an exponential rise. This is caused not only by the above-described points, but also by feedback effects as further described below.

How much will temperatures rise?
In the above graph, rising temperatures are compared to the global average for the period 1951-1980, which is typically used as a base period by NASA in temperature change analysis. The background behind this is that the U.S. National Weather Service uses a three-decade period to define "normal" or average temperature. The NASA Goddard Institude for Space Studies (GISS) analysis of temperature anomalies began around 1980, so the most recent 30 years at the time was 1951-1980.

The study 'Climate Impact of Increasing Atmospheric Carbon Dioxide', by NASA scientists led by James Hansen, describes those early efforts and was published in Science back in 1981. The image below is from the paper, showing that much of the extra heat trapped by carbon dioxide released by people in the atmosphere ends up in oceans.


The paper discusses how many years it can take for oceans to warm up, and the role of feedbacks in that process. The paper notes that a surface albedo change over land areas of 5% (equivalent to a 1.5% global change), would affect global temperature by 1.3°C, adding that paleclimatic evidence suggests that surface warming at high latitudes will be two to five times the global mean warming, due to snow/ice albedo feedback and greater atmospheric stability, which magnifies the warming of near-surface layers.

Feedbacks further accelerate warming in the Arctic

Feedbacks are described in more detail in posts such as Diagram of Doom (image below) and Changes to Polar Vortex affect mile-deep ocean circulation patterns.

Diagram of Doom
One such feedback is albedo change — retreat of Arctic sea ice results in less sunlight being reflected back into space, as further discussed in Albedo Change in the Arctic. Loss of Arctic sea ice is effectively doubling mankind's contribution to global warming. Increased absorption of the sun's rays is the equivalent of about 20 years of additional CO2 being added by man, Professor Peter Wadhams said in a BBC article.

One of the most threatening feedbacks is release of methane that are held in the currently frozen seabed. As the seabed warms up, it starts to release methane in what can be rather abrupt ways. Due to methane's high global warming potential and low levels of hydroxyl in the Arctic, this threatens to further accelerate local warming and trigger further methane releases, in a vicious spiral of runaway global warming.

from: Methane Hydrates

This situation calls for comprehensive and effective action as discussed at the climateplan blog.

Related

- Accelerated Warming in the Arctic 

- Arctic Ocean is turning red

- How much will temperatures rise?

- Methane Hydrates

Stop All New Fossil Fuel Megaprojects



Why is Obama not rejecting the Keystone XL pipeline now?

In light of Obama's 42 minute climate change speech, his understanding on the lack of permanent jobs created, as well as his knowledge on the corrupted environmental assessment report generated by pipeline advocates, one has to wonder what the delay is for? Clearly, Obama will reject the pipeline or completely lose support and credibility and destroy his long-term legacy.

So why the delay? For one thing, other pipelines are being planned and designed and pretty much slipped under the radar. Like the reversal of Enbridge Line 9 and conversion from natural gas to dilbit and a capacity of 1.1 million barrels per day, much higher than the 0.85 mbd from Keystone XL. By delaying on the Keystone XL, Obama is keeping pressure off these other projects which are threatening to slip in under the radar while people opposed are preoccupied with the Keystone XL.

This needs to change. People opposed to Keystone XL need to ramp up their opposition to all pipeline projects, in fact to all new fossil fuel megaprojects, including coal and pipelines and tankers and also to fracking. The reason is that climate change has moved into a much more rapid and abrupt regime, whereby massive extreme weather events like torrential rains cause floods in some regions, and long-term persistent droughts occur in other regions, all at the whim of a wavy and stuck jet stream.


Paul Beckwith is a part-time professor with the laboratory for paleoclimatology and climatology, department of geography, University of Ottawa. He teaches second year climatology/meteorology. His PhD research topic is “Abrupt climate change in the past and present.” He holds an M.Sc. in laser physics and a B.Eng. in engineering physics and reached the rank of chess master in a previous life.


Related

- The Social Tipping Point - by Paul Beckwith
http://arctic-news.blogspot.com/2013/08/the-social-tipping-point.html

- The Obama Climate Plan: Disappointing and Hopeless - by Peter Carter
http://arctic-news.blogspot.com/2013/07/the-obama-climate-plan-disappointing-and-hopeless.html

- Comprehensive and Effective Climate Plan - by Sam Carana

Thursday, August 15, 2013

Arctic Sea Ice in Free Fall

Arctic Sea Ice has declined dramatically recently. The recent image below, by the Danish Meteorological Institute, shows the decline in extent over the past few days, with extent calculated by including all areas with ice concentration higher than 30%.


As the above image shows, sea ice extent (30%+ concentration) is now lower than any other year, except 2007 and 2012. Moreover, the sharp decline looks set to continue.

Ice volume and concentration have dropped dramatically, partly as a result of the cyclone that hit the Arctic Ocean a few days ago. The eye of the cyclone is still visible almost exactly above the North Pole on the Naval Research Laboratory image below on the right, where sea ice concentration appears to form a circle.

The sea ice looks set for an all-time record low; all this thin ice looks set to disappear over the next few weeks.

The graph below, also by the Danish Meteorological Institute, calculates sea ice extent by including all areas with 15% or more ice concentration.
The above graph also shows a steep recent descent, although not as pronounced as in the graph at the top that includes spots with 30% or more ice concentration. The graph at the top better illustrates recent drops in ice concentration from, say, 40% to 20%, which can occur quite abruptly due to the impact of a cyclone. 

The Danish Meteorological Institute has meanwhile produced a more recent version of the graph based on spots with 30% or more ice concentration (added below).


The above graph shows an August 15 extent that appears to be back in line with the earlier trend. At first glance, it may appear as if the sea ice has largely recovered from the impact of three cyclones that have hit the Arctic Ocean over the past two months. 

However, these cyclones are likely to have contributed to the appearance and persistence of thin spots in the ice close to the North Pole. This phenomenon was earlier described in posts such as Thin Spots developing in Arctic Sea Ice

The conclusion remains the same as the one drawn then in that post, i.e. that for years, observation-based projections have been warning about Arctic sea ice collapse within years, with dire consequences for the Arctic and for the world at large.

Cyclones can speed up this collapse. On this point, it's good to remember what Prof. Peter Wadhams said in 2012:
". . apart from melting, strong winds can also influence sea ice extent, as happened in 2007 when much ice was driven across the Arctic Ocean by southerly winds (not northerly, as she stated). The fact that this occurred can only lead us to conclude that this could happen again. Natural variability offers no reason to rule out such a collapse, since natural variability works both ways, it could bring about such a collapse either earlier or later than models indicate.

In fact, the thinner the sea ice gets, the more likely an early collapse is to occur. It is accepted science that global warming will increase the intensity of extreme weather events, so more heavy winds and more intense storms can be expected to increasingly break up the remaining ice, both mechanically and by enhancing ocean heat transfer to the under-ice surface."
Hopefully, more people will realize the urgency of the situation and realize the need for a comprehensive and effective plan of action as described here.