Blog Archive

Tuesday, November 10, 2009

The Leadership Campaign celebrates the presence of James Hansen at their sleepout protest on Boston Common

Dear Readers,

I am so happy to see young people get involved.  Here are some tidbits from the Leadership Campaign of Massachusetts:

SHHHH…

Posted in Uncategorized on November 9, 2009 by Tufts University
James Hansen is sleeping in our tent!
Observe:
JamesfingHansen
-Tufts

JAMES HANSEN – TODAY at 350pm

Posted in Uncategorized on November 8, 2009 by Jay O'Hara Alright everybody, are you ready to take this to the next level?  Tonight and tomorrow is destined to be the biggest and most exciting sleep-out yet.  Here’s why: Dr. James Hansen, lead climate scientist at NASA will be sleeping out with us tonight and testifying before the Senate Global Warming Committee on Monday.
Grab your sleeping bag, grab your hat and head on down to the Commons.  This is going to be awesome.  Here’s the schedule of events:
Dr. James HansenWhen: Sunday, November 8th
Where: Boston Common, in front of the Statehouse
3:50pm: Rally on Boston Common
5:30pm: Tent set up
Monday, November 9
8:00am: Wake up, pack up tents
10:00am: Senate Committee on Global Warming and Climate Change Hearing with Dr. James Hansen, Bishop Bud Cederholm, Economist Frank Ackerman, and student leader Dominique McCadden.
Join the Facebook event, follow our Twitter feed and we’ll see you there!

Link to blog:   http://theleadershipcampaign.wordpress.com/

Dr. James Hansen rallies and testifies for 100% clean electricity in Massachusetts


Dr. Hansen receiving a citation at 3 a.m. for sleeping in a city park.


DR. JAMES HANSEN RALLIES AND TESTIFIES FOR 100% CLEAN ELECTRICITY IN MA


The Leadership Campaign, November 9, 2009


Boston, MA -- Dr. James Hansen joined the Leadership Campaign Sunday and Monday to rally for 100% clean electricity in Massachusetts.  He joined with 155 Leadership Campaign (The LC) participants on the Boston Common for the third consecutive Sunday sleep-out.  They are refusing to sleep in their homes powered by dirty electricity until there is a plan in place to power them by clean electricity.



Dr. Hansen and The LC are calling on Massachusetts to pass a bill that will re-power the State with 100% clean electricity in ten years. Dr. Hansen took a train up Sunday morning to rally and sleep-out with the participants even as he recovers from surgery.   He rallied and slept-out Sunday.  Monday morning he testified at an informational hearing sponsored by the Senate Committee on Global Warming and Climate Change.

Last week twelve Boston police officers roused all sleepers at 3:00AM to take down each person's identification.  It is still unclear whether or not they will be receiving citations for trespassing on Boston Common after hours.  Last night, five police officers gave the participants two minutes to leave or citations would be issued.  Approximately 80 people volunteered themselves for citations, including Dr. Hansen. 



Sunday's rally encompassed the necessity of creating  climate policy that follows the most up-to-date and accurate climate science. Speakers other than James Hansen included: Marla Marcum of Mass. Council of Churches; Linnea Palmer Paton, student of Worcester Polytechnic Institute; Alex Propp, student at Amherst College; Steve MacAusland, co-founder of the National Interfaith Power & Light Movement; Ken Ward of the JP Greenhouse; State Representative Will Brownsberger, Vice-Chair of House Global Warming and Climate Change Committee; and Craig Altemose, Harvard graduate student and Coordinator of The Leadership Campaign. 


Rep. Brownsberger said, " ...Americans are stuck out there in suburbia eating what the corporate food system feeds them.  It's not enough to do the right thing in our personal lives - we have to engage in social action, and that is what you are doing today."


"Our universe is incredibly unjust and inequitable for young people and future generations. " Dr. Hansen said.  "Unless someone can change the direction, young people are really in trouble.  Our governments are not taking actions or planning actions that will achieve this."

Today Dr. Hansen testified in front of an informational hearing sponsored by the Senate Committee on Global Warming and Climate Change.  He testified with Frank Ackerman, Senior Economist at Stockholm Environment Institute; Rt. Reverand Roy Cederholm, Jr., Bishop Suffragan of the Episcopal Diocese of Massachusetts; and Dominique McCadden, a student from Northeastern University and participant of The Leadership Campaign.  There was an opportunity for question and answer at the press conference immediately following the hearing.

Hansen began his testimony by saying he wanted to, "plant in the mind a seed - ways Massachusetts can exercise leadership and show the rest of the U.S. kinds of actions that are needed to combat climate change, and that they are possible."  He went on to say, "When we hear politicians say they understand the planet is in peril and they will do something about it - they are not telling the truth.  They are allowing us to go down a path that will give young people and future generations a problem they cannot solve." 



Bishop Cederholm discussed the morality issue on our state's leadership on the climate crisis.  "Massachusetts has and needs to continue to be a leader," He said. "If we don't, who will?  We hope the legislature in this state will answer with: we will. For the sake of generations to come."



Also at this hearing, Senator Marc Pacheco publicly announced his support for The Leadership Campaign's ask.  "We need to have 100% clean electricity within the next ten years." 


The Leadership Campaign is a movement run by Students for a Just and Stable Future, a network of college students across the Commonwealth of Massachusetts advocating for serious and practical solutions to global climate disruption. Find out more on their website,www.theleadershipcampaign.org and follow their blog at:www.theleadershipcampaign.wordpress.com.

  • Upcoming Events

    • 11/15 5:00 p.m. March from M-CAN Conference at MIT with Bill McKibben
    • 11/15 6:00 p.m. Rally on Boston Common with Bill McKibben
    • 11/16 9:00 a.m. Lobby Day at State House
    • 12/7, Copenhagen Conference begins


Contact: Dan Abrams, dabrams@masspowershift.org, (518) 527-9168; or Craig Altemose, caltemose@masspowershift.org, (201) 841-7105




Mauri Pelto on Real Climate: Is Pine Island Glacier the Weak Underbelly of the West Antarctic Ice Sheet?

Is Pine Island Glacier the Weak Underbelly of the West Antarctic Ice Sheet?

— eric @ 9 November 2009:  Guest post by Mauri Pelto on Real Climate

AntarcMapPelto 
It is popularly understood that glaciologists consider West Antarctica the biggest source of uncertainty in sea level projections. The base of the 3000-m thick West Antarctic Ice Sheet (WAIS) – unlike the much larger East Antarctic Ice Sheet – lies below sea level, and it has been recognized for a long time that this means it has the potential to change very rapidly. Most of the grounded West Antarctic ice sheet drains into the floating Ross and Ronne-Filchner ice shelves, but a significant fraction also drains into the much smaller Pine Island Glacier. Glaciologists are paying very close attention to Pine Island Glacier (”PIG” on map, right) and nearby Thwaites Glacier. In the following guest post, Mauri Pelto explains why.

In science there are instances when a specific mechanism is understood and a hypothesis posed based on an understanding of the processes involved, prior to the initiation or observation of the those processes. An excellent example is the determination by Molina and Rowland (1974) that CFC’s will lead to losses in stratospheric ozone. The full truth of their understanding of the process was not revealed until the Antarctic ozone hole was reported in 1985 by Farman et al.

A different example, from the same time period, was the 1978 publication by the late John Mercer, Ohio State U., who argued that a major deglaciation of the West Antarctic Ice Sheet (WAIS) may be in progress within 50 years. This conclusion was based on the fact that the WAIS margin was ringed with stabilizing ice shelves, and that much of the ice sheet is grounded below sea level. The loss of ice shelves — Mercer proposed — would allow the ice sheet to thin, grounding lines to retreat and the ice sheet to disintegrate via calving. This is a much faster means of losing mass than melting in place. Mercer further commented that the loss of ice shelves on the Antarctic Peninsula, as has since been observed, would be an indicator that this process of ice sheet loss due to global warming was underway.

Mercer’s ideas led Terry Hughes (1981) (my doctoral advisor at U. of Maine) to propose that the WAIS had a “weak underbelly” in Pine Island Bay. This bay in the Amundsen Sea is where the Pine Island Glacier (PIG) and Thwaites Glacier reach the sea. These are the only two significant outlet glaciers draining the north side of the WAIS. Together they drain 20% of the WAIS. Hughes called this area the “weak underbelly” because these glaciers lack the really huge ice shelves Ross Ice Shelf and the Ronne-Filchner Ice Shelf in which most other large WAIS outlet glaciers terminate. Both glaciers have a relatively rapid flow from the WAIS interior to the calving margin. Further the low surface slopes and smooth flow patterns of PIG suggested to Hughes that there was no indication of a landward rise in the elevation of the glacier bed; such a rise would help stabilize the glacier. Without a rise in the bed, glacier thinning and retreat could result in continual grounding line retreat. The grounding line is where the bottom of the glacier comes in contact with the ground below the ice sheet, in this case the sea bottom. The grounding line is an anchoring point for the outlet glaciers. The length of the glacier that is grounded is both slowed and stabilized by resulting basal friction. Beyond the grounding line toward the margin, the floating ice shelf is susceptible to rapid calving retreat and as the grounding line retreats, so would the calving front. Note in the image below that the situation is even less stable than Hughes speculated. The current grounding line is at a higher elevation than the bed of the glacier for the next 200 km inland of this grounding line. (Note, inland is to the left in the figure, below.) The deeper the basin, the thicker the ice must be to maintain grounding. This makes it tough to slow grounding line retreat once it begins in a deepening basin.
Pine-Is-Glacier4
Basal topography profile of Pine Island Glacier (from Shepherd et al., 2001)
The weak underbelly idea was forgotten for some time. While I was attending a conference on rapid glacier flow in Vancouver BC in 1986, data were presented that showed no acceleration of Pine Island Glacier. This was further noted for the entire 1970’s to early 1990’s period by Lucchita and others (1995).

Then, in 1998, Rignot (1998) used satellite imagery to identify that the grounding line of Pine Island Glacier had retreated 5 km from 1992 to 1996. In the same year, Wingham and others (1998) observed a 10 cm per year thinning in the drainage basins for Thwaites and PIG during the 1990’s. Shepherd and others (2001) noted thinning in the fast flow areas of the glacier of 1.6 m/year between 1992 and 1999. This led them to conclude that the observed inland thinning and acceleration of PIG was a response to enhanced glacier bed lubrication. Not from surface melting of course as there is next to none on this glacier. Rignot and others (2002) noted that the glacier had accelerated 18% over a 150 km long section of the glacier in the fast flow area between 1992 and 2000. Change was afoot: after 50 years of apparent stability, the glacier calving front was retreating, and the grounding line was retreating indicating reduced bedrock anchoring. The reduction in basal friction would then lead to faster flow and more thinning. Was this just a short-term increase?

In 2006 and 2007, instruments were placed directly on PIG for the first time by the British Antarctic Survey. Four GPS receivers monitored ice flow from 55 to 171 km inland of the calving front at the center of the glacier (Scott and others, 2009). Glacier velocities had been noted at each site in 1996; by 2007 the respective increase in velocity was 42%, 36%, 34% and 26% respectively, an approximately 2 to 3% annual increase. The increase from 2006 to 2007 was 6.4% at 55 km from the terminus and 4.1% at 171 km inland. The extent of the fast flowing portion of PIG is seen in the figure below. A separate data set, radar based was used by Rignot (2008) to identify a 42% acceleration of PIG between 1996 and 2007 accompanied by most of its ice plain becoming ungrounded.

PIG_TG
Velocity map of Pine Island and Thwaites Glaciers. Rignot, 2008

Scott and others (2009) pointed out that the greater thinning toward the grounding line and terminus increased the surface slope and the gravitational driving stress, further promoting acceleration. Then Wingham and others (2009) reported that the 5400 km² central trunk of the glacier had experienced a quadrupling in the average rate of volume loss quadrupling from 2.6 km3 a year in 1995 to 10.1 km3 a year in 2006. PIG had an annual volume flux at the front of 28 km3 a year, so this increase is a marked change. Their observations were that the region of lightly grounded ice at the glacier terminus is extending upstream, and the changes inland are consistent with the effects of a prolonged disturbance to the ice flow, such as the effects of ocean-driven melting. Further examination of the bed topography by Vaughan and others (2006) indicates that most of the bed of the drainage basin of PIG is more than 500 meters below sea level, and there is a particularly deep basin in the eastern section of the upper basin. The observed acceleration, retreat of the grounding line, thinning of the lower section of the glacier, and the observed elevation of the basal topography provide no indication that this is not a weak underbelly of WAIS.

The evidence does indicate that one of the basic underlying principles, proposed by Mercer and Hughes, of what can stabilize or destabilize WAIS was right on the money. The evidence reviewed does not fully confirm the weak underbelly hypothesis, but it provides enough evidence that we had best monitor the situation and expand our attempts to understand it. That is just what the glaciological and scientific community are doing. A number of projects from the British Antarctic Survey, NASA and NSF will continue to expand the research in the area. In January 2008 Robert Bindschadler (NASA) landed on the floating ice shelf of PIG. They found the situation hazardous for plane landing but did leave behind several instruments. NSF has decided to fund establishment of a helicopter camp to safely study the ice-ocean interaction during the 2010-11 summer field season in Antarctica. In 2009 a team of British and American scientists deployed an autonomous robot submarine on six missions beneath the PIG ice shelf using sonar scanners to map the seabed and the ice shelf bottom. This fall NASA’s Operation Ice Bridge has focused much of its energy on the Pine Island Glacier. Seelye Martin of the University of Washington notes that “Pine Island Glacier is a major focus for our mission. We have four flights planned for this glacier. One of our hopes with these flights is to understand the detailed topography under the floating ice tongue. That topography controls the rate of melting there.”

PIGBasal
Basal topography of Pine Island Glacier region (from Vaughan et al, 2006).

Link to this Real Climate blog post:  http://www.realclimate.org/index.php/archives/2009/11/is-pine-island-glacier-the-weak-underbelly-of-the-west-antarctic-ice-sheet/

A. Laurian et al., GRL 36 (2009), Global surface cooling: The atmospheric fast feedback response to a collapse of the thermohaline circulation

Geophysical Research Letters, 36 (2009) L20708; doi: 10.1029/2009GL040938.

Global surface cooling: The atmospheric fast feedback response to a collapse of the thermohaline circulation

A. Laurian, S. S. Drijfhout, W. Hazeleger and R. van Dorland (Royal Netherlands Meteorological Institute, De Bilt, Netherlands)

Received 10 September 2009; accepted 24 September 2009; published 28 October 2009.

Abstract 

In the ECHAM5/MPI-OM model a collapse of the Atlantic thermohaline circulation results in a global surface cooling of 0.72 K. The mechanisms that are responsible for this cooling are investigated. Additional experiments were performed with a one-dimensional radiative convective model in which anomalies from the climate model were prescribed. Fast atmospheric feedbacks are essential to maintain and strengthen the global surface cooling caused by a THC collapse. Reduced downward long wave radiation exceeds the decreased upward long wave radiation. This decreased downward long wave radiation is caused by reduced water vapor content rather than by ice-albedo feedbacks. Also, the decrease in water vapor is much stronger than suggested by the water vapor feedback expected from the simulated albedo change. The large decrease in water vapor is the main feedback. On the regional scale, changes in cloud water and cloud radiative forcing further modify the surface cooling.

Extraordinary September Arctic sea ice reductions and their relationships with storm behavior over 1979–2008

Geophysical Research Letters, 36 (2009) L19715; doi: 10.1029/2009GL039810.

Extraordinary September Arctic sea ice reductions and their relationships with storm behavior over 1979–2008

Ian Simmonds and Kevin Keay (School of Earth Sciences, The University of Melbourne, Victoria, Australia)

Received 29 June 2009; accepted 1 September 2009; published 14 October 2009

Abstract

Dramatic changes have been observed in Arctic sea ice, cyclone behavior and atmospheric circulation in recent decades. Decreases in September ice extent have been remarkable over the last 30 years, and particularly so in very recent times. The analysis reveals that the trends and variability in September ice coverage and mean cyclone characteristics are related, and that the strength (rather than the number) of cyclones in the Arctic basin is playing a central role in the changes observed in that region, especially in the last few years. The findings reinforce suggestions that the decline in the extent and thickness of Arctic ice has started to render it particularly vulnerable to future anomalous cyclonic activity and atmospheric forcing.

M. D. Palmer, S. A. Good, K. Haines, N. A. Rayner & P. A. Stott, GRL 36 (2009), A new perspective on warming of the global oceans

Geophysical Research Letters, 36 (2009) L20709; doi: 10.1029/2009GL039491.

A new perspective on warming of the global oceans

M. D. Palmer, S. A. Good (Met Office Hadley Centre, Exeter, U.K.), K. Haines (Environmental Systems Science Centre, University of Reading, Reading, U.K.), N. A. Rayner and P. A. Stott (Met Office Hadley Centre, Exeter, U.K.)

Received 5 June 2009; accepted 31 August 2009; published 29 October 2009

Abstract

Changes in ocean circulation associated with internal climate variability have a major influence on upper ocean temperatures, particularly in regions such as the North Atlantic, which are relatively well-observed and therefore over-represented in the observational record. As a result, global estimates of upper ocean heat content can give misleading estimates of the roles of natural and anthropogenic factors in causing oceanic warming. We present a method to quantify ocean warming that filters out the natural internal variability from both observations and climate simulations and better isolates externally forced air-sea heat flux changes. We obtain a much clearer picture of the drivers of oceanic temperature changes, being able to detect the effects of both anthropogenic and volcanic influences simultaneously in the observed record. Our results show that climate models are capable of capturing in remarkable detail the externally forced component of ocean temperature evolution over the last five decades.


Citation: Palmer, M. D., S. A. Good, K. Haines, N. A. Rayner, and P. A. Stott (2009), A new perspective on warming of the global oceans, Geophys. Res. Lett., 36, L20709, doi:10.1029/2009GL039491.

S. Jevrejeva, A. Grinsted & J. C. Moore, GRL 36 (2009), Anthropogenic forcing dominates sea level rise since 1850

Geophysical Research Letters, 36 (2009) L20706; doi: 10.1029/2009GL040216.

Anthropogenic forcing dominates sea level rise since 1850

S. Jevrejeva (Proudman Oceanographic Laboratory, Liverpool, U.K.), A. Grinsted (Centre for Ice and Climate, Niels Bohr Institute, University of Copenhagen, Copenhagen, Denmark), J. C. Moore (Arctic Centre, University of Lapland, Rovaniemi, Finland; Thule Institute, University of Oulu, Oulu, Finland; College of Global Change and Earth System Science, Beijing Normal University, Beijing, China)

Received 23 July 2009; accepted 23 September 2009; published 28 October 2009

Abstract

The rate of sea level rise and its causes are topics of active debate. Here we use a delayed response statistical model to attribute the past 1000 years of sea level variability to various natural (volcanic and solar radiative) and anthropogenic (greenhouse gases and aerosols) forcings. We show that until 1800 the main drivers of sea level change are volcanic and solar radiative forcings. For the past 200 years sea level rise is mostly associated with anthropogenic factors. Only 4 ± 1.5 cm (25% of total sea level rise) during the 20th century is attributed to natural forcings, the remaining 14 ± 1.5 cm are due to a rapid increase in CO2 and other greenhouse gases.

Link to abstract:  http://www.agu.org/pubs/crossref/2009/2009GL040216.shtml

NOAA: Report on October 2009 in the Contiguous States -- Precipitation Highlights

Dear Readers,

Below you will read that October was the wettest month in most of the U.S. for the past 167 years.

Here in Brazil, October was the wettest month in most regions for the past 67 years of record keeping.

I can attest to this because a couple of weeks ago, we had a downpour here that was more than the usual combined total for the entire month of October -- 15 inches in one night!

Tenney

  • Precipitation Highlights - October 2009
  • The U.S. recorded its wettest October in the 115-year period of record. The nationwide precipitation of 4.15 inches was nearly double the long-term average of 2.11 inches.
  • Regionally, two of the nation's nine climate regions (the East North Central and South) saw their wettest October. The Central region had its second wettest October, while the West North Central had its fourth wettest. This was the first month since December 2007 that no region had below normal precipitation.
  • Three states (Iowa, Arkansas, and Louisiana) saw their record wettest October. Fourteen other states had precipitation readings ranking in their top five category. Only three states (Florida, Utah, and Arizona) saw below normal precipitation.
  • Arkansas continued its remarkable run of wetness in 2009. The state has seen four months with top three precipitation ranks this year (May, 1st wettest; July, 3rd wettest; September, 2nd wettest; October, 1st wettest). As a result, the state's year-to-date average is the wettest in 115 years of record keeping. This contrasted with persistent dryness in Arizona, which saw its second-driest year-to-date period.
  • The three-month (August-October) rainfall was record-setting for many adjacent divisions within Texas, Louisiana, Arkansas, Mississippi, Alabama, and Georgia. It is noteworthy that this occurred despite only one tropical cyclone (Claudette, in August) making landfall in the region during this period.
  • By the end of October, moderate-to-exceptional drought covered 12% of the contiguous United States, the second-smallest drought footprint of the decade, based on the U.S. Drought Monitor. Major drought episodes in California and South Texas improved significantly. Drought conditions emerged across much of Arizona.
  • About 45% of the contiguous United States had moderately-to-extremely wet conditions at the end of October, according to the Palmer Index (a well-known index that measures both drought intensity and wet spell intensity). This is the largest such footprint since February 2005.
  • Other Items of Note
  • According to the NOAA Midwest Regional Climate Center in Champaign, Illinois, more than half of the long-term stations in the Midwest had one of their five wettest Octobers on record, with one out of five observing its wettest. Combined with the cold, this delayed crop planting and stunted crop maturity. Corn development was as much as four weeks behind in places, and the soybean harvest was well behind schedule throughout the region.
  • Two major snow storms hit the contiguous United States during October. The first struck the Upper Midwest October 9th through 13th, while the second blanketed the western Plains States October 27th through 30th. By month's end, 13.6 percent of the nation was under snow cover, according to NOAA's National Operational Hydrologic Remote Sensing Center.
  • Unusually cold and wet conditions across the middle of the country led to several snowfall records. Cheyenne, Wyoming observed 28 inches of snow during October, making this the city's snowiest October on record. North Platte, Nebraska recorded 30.3 inches of snowfall, making October 2009 the snowiest month of all months on record for the city. The previous record was 27.8 inches, in March 1912.
  • October, like September, saw below-normal fire activity in all respects. A total of 3,207 fires burned about 158,000 acres in October, according to the National Interagency Coordination Center. Each of these values is below this decade's average for October.

Alaska:
  • Alaska had its 10th warmest October since records began in 1918, with a temperature 6.3 °F (3.5 °C) above the 1971–2000 average.

  • Alaska had its 15th warmest August–October on record, with a temperature 2.2 °F (1.2 °C) above the 1971–2000 average.

  • Alaska had its 22nd warmest January–October on record, with a temperature 0.9 °F (0.5 °C) above the 1971–2000 average.
For additional details about recent temperatures and precipitation across the U.S., see the Regional Highlights section below and visit the Climate Summary page. For information on local temperature and precipitation records during the month, please visit NCDC's Records page. For details and graphics on weather events across the U.S. and the globe please visit NCDC's Global Hazards page.

Lou Grinzo: James Hansen speaks

James Hansen speaks

by Lou Grinzo, theenergycollective.com, November 11, 2009

James Hansen has posted a couple of very interesting items, albeit interesting for different reasons, on his web site.

The first is his letter, I Just Had a Baby, at Age 68 [PDF], which details his recent experience with prostate cancer surgery, and talks about his participation in a “sleep out” event outside the Massachusetts State House.

The second is a copy of his presentation from the end of October to the Club of Rome General Assembly, Global Warming Time Bomb: Actions Needed to Avert Disaster [PDF].

I was pleasantly surprised to see Hansen talk so prominently in this presentation about the knowledge gaps regarding what is understood (by scientists) and what is known (by the public and policymakers). After the way I’ve been blithering on about the two “cognitive gaps” for so long, with basically no feedback from anyone, I’m quite relieved to see someone of Hansen’s stature prove that I wasn’t imagining it all. (Or if I was, then so is Hansen, and I’m still in good, albeit delusional, company.)

Some snippets from the speaker’s notes (included in the PDF linked above):
Here are several climate tipping points of special concern. Tipping points are “non-linear” phenomena, which means that they can reach a point at which rapid catastrophic change occurs. It is inherently difficult to determine the time at which non-linear collapse will occur, even in cases where such rapid change is certain.
The mechanism that seems to be most important for disintegration of the great ice sheets that cover Antarctica and Greenland begins with ocean warming. Ocean warming leads to melting of ice shelves, which are tongues of ice that stretch out into the ocean. The ice shelves buttress the ice sheets, so when ice shelves disappear the more mobile parts of the ice sheet, the ice streams, can surge into the ocean – thus removal of the ice shelves is somewhat akin to taking the cork out of a bottle – it allows the material behind to flow rapidly. We know from Earth’s history that once ice sheet disintegration is well underway, sea level can rise by several meters per century.
Species extermination is also a non-linear problem. Today we are placing many species under multiple stresses, but one stress that is growing rapidly is the shifting of climate zones due to global warming. An average temperature line has been moving poleward at a rate of 50-75 kilometers per decade during the past three decades. As the total movement of climate zones becomes larger it threatens those species that are less mobile. Because of interdependencies of species, the loss of key species can cause entire ecosystems to collapse.
Methane is an especially powerful greenhouse gas. There are large amounts of methane presently locked up, frozen, in high latitude tundra and, especially, in ocean sediments on continental shelves. We know from Earth’s history that this frozen methane can be released suddenly by sufficient warming – thus this methane has the potential to greatly amplify humanmade global warming, if that warming reaches a level, a tipping point, such that large volumes of frozen methane begin to melt.

Arctic sea ice is another potential tipping point of the climate system. The area of sea ice at the end of the summer began to be measured accurately from satellites in the late 1970s. The graph shows that the area of sea ice fluctuates from year to year, based on variable weather patterns. However, overall there has been a decline in sea ice area over the past three decades. In 2007 there was a sharp decline of sea ice area, to an amount just over half of the ice area three decades earlier.

Although sea ice recovered slightly in 2008 and even more in 2009, most analyses indicate that all summer sea ice will be lost within the next few decades, if business-as-usual greenhouse gas increases continue. It is difficult to imagine that the Greenland ice sheet could survive, if the Arctic sea ice disappears in summer.
Stabilization of Arctic sea ice requires, to first approximation, that Earth’s energy balance is restored. At present, because human-made greenhouse gases have reduced the amount of heat radiation that Earth is emitting to space, the planet is out of energy balance by about 0.5 watts per square meter, uncertain by about 0.25 watts per square meter. Other things being equal, the amount of carbon dioxide in the air would need to be reduced from its present 387 ppm (parts per million) to about 350 ppm in order to increase emission of heat radiation to space by 0.5 watts per square meter and restore Earth’s energy balance.

I will emphasize the intergenerational inequity of global warming. This is a photo of our first grandchild, taken several years ago. Some newspapers had described me as the grandfather of global warming, so for amusement I showed this photo – I really was a grandfather.
My grandchildren began to influence me when I realized that policy makers were ignoring the message from the climate science – or rather that politicians were developing the fine art of greenwash – they would say favorable words about the environment and stabilizing climate – but their actions were inconsistent with that goal. Politicians would be happy if scientists just tell them there is a climate problem and then go away and shut up – let them decide what they want to do. But I decided that I did not want my grandchildren, some day in the future, to look back and say “Opa understood what was happening, but he did not make it clear.”

What is clear is that we cannot burn all the fossil fuels. There is a limit on how much carbon we can put into the atmosphere.
These graphs [see original document] tell us unambiguously that we must phase out all coal emissions rapidly, not develop the unconventional fossil fuels, and not even go after every last drop of oil on the planet. In that case, our children and grandchildren have a chance of inheriting a planet that is not spiraling out of their control.
As I’ve been saying for some time, climate change will “save us” from peak oil, not the other way around. Of course, in this case “save us” is akin to a ship’s captain chopping a hole in the bottom of his boat so that his crew will have to constantly bail water and thereby not drown to death.

Link:  http://theenergycollective.com/TheEnergyCollective/51278

Removing Coal River Mountain

Removing Coal River Mountain

Removing Coal River Mountain
The message was like a punch in the gut: "The blasting has begun."

Coal River Mountain in southern West Virginia, heretofore America's "most endangered" mountain, is now under assualt by Massey Energy, the nation's fourth-largest coal company and the worst offender when it comes to the worst coal mining there is -- mountaintop removal.

Starting with that email from Appalachian Voices late on Friday, and continuing with a flurry of messages over the weekend, it appears that the heavy equipment on top of Coal River Mountain is now operating and the blasting has begun.  (Jeff Biggers provides exclusive photos on his blog.)  Massey's mountaintop removal operation would destroy over 6,000 acres of Coal River Mountain, wipe out 10 square miles of lush forests, create 18 valley fills, devastate the Clear Fork watershed, and ruin the lives of local residents who have been fighting valiantly to defend the homeland they hold so dear.

Bear in mind that the company is detonating high-explosives close to the notorious Brushy Fork impoundment, an enormous earthen retention pond holding more than 8 billion gallons of toxic coal slurry waste.  This impoundment is just up the valley beyond the Shumate Dam (pictured below), which also holds back billions of gallons of coal sludge and is perched just a few hundred yards above Marsh Fork Elementary School.

If the blasting on Coal River Mountain causes the Brushy Fork pond to rupture, the resulting sludge flash-flood could threaten the lives of people living downstream.

Aside from that obvious disaster, the mining means the death of an alternative energy project that would be a win-win for the community.  You see, Coal River Mountain has the highest peaks ever slated for mining in the state of West Virginia.  According to a study conducted for Coal River Wind, this mountain is an ideal location for a commercial-scale clean energy project that would protect the environment while providing more jobs than Massey's coal mining operation.  But a leveled mountain means the loss of elevation that would power those wind turbines.

To date, West Virginia's governor, Joe Manchin, has rejected the pleas of local residents to save the mountain by supporting the wind project.  Other elected officials have also side-stepped the controversy.  Given that the Obama administration has taken tentative steps toward curtailing mountaintop removal in Appalachia, perhaps the last, best hope for Coal River Mountain lies in Washington, D.C.

Please take a moment to call President Obama today at 202-456-1414 and implore him to mobilize federal agencies to stop the senseless destruction of Coal River Mountain immediately.

Link:  http://switchboard.nrdc.org/blogs/rperks/removing_coal_river_mountain.html

Monday, November 9, 2009

Sea level rise along coast of western Australia almost triple the global average at 8.6 mm/yr instead of 3.2 mm


Western Australia sea level rising fast, at almost triple the global average

by Phil Mercer, BBC News, Sydney, November 9, 2009


Cottesloe Beach, Perth, WA, 2007
Perth's beaches are key to city life, but sea levels are rising fast
New figures have revealed that sea levels along the coast of Western Australia are rising at a rate double that of the world average.
Statistics from Australia's National Tidal Centre show levels have increased by 8.6 mm a year off the coast of the state capital Perth.
That compares to a global average of just over 3 mm.
Scientists have said that man-made climate change has played a significant role in the rise.
Climatologists have said that a combination of natural variability and man-made pollution have caused sea levels to rise around the world.
Double trouble
For much of the past century there were average increases of 1.7 mm per year, while that rate doubled after 1993.
Some regions, however, have suffered more than others.
New figures show that the sea level rose off Perth in Western Australia and in the Kimberley region to the north by more than 8 mm.
Dr John Church, from Australia's government-funded science and research body, the CSIRO, says these are worrying signs.
"Man's role is making a significant contribution to this global average rise," he said.
"I think the fact that sea levels are rising is a major reason for concern and it's a combination of the global average rise together with the natural variability leading to larger regional rises over certain periods and extreme events as in storm surges which will have the most impact…and, of course, sea level rise will not stop in 2100, it will continue for many centuries," he added.
About 80% of Australians live in coastal areas.
There are fears that vulnerable low-lying communities may have to be abandoned in years to come because of flooding and erosion.
CSIRO scientists have said that warming temperatures, which cause water to expand, have been a major trigger for sea-level rises in the 20th Century.
They have also blamed the melting of the world's icecaps and glaciers.

Link to article on BBC: http://news.bbc.co.uk/2/hi/asia-pacific/8349760.stm

Interactions with aerosols boost warming potential of some gases

Interactions with aerosols boost warming potential of some gases


NASA's Earth Observatory, October 29, 2009

For decades, climate scientists have worked to identify and measure key substances -- notably greenhouse gases and aerosol particles -- that affect Earth’s climate. And they’ve been aided by ever more sophisticated computer models that make estimating the relative impact of each type of pollutant more reliable.

Yet the complexity of nature -- and the models used to quantify it -- continues to serve up surprises. The most recent? Certain gases that cause warming are so closely linked with the production of aerosols that the emissions of one type of pollutant can indirectly affect the quantity of the other. And for two key gases that cause warming, these so-called “gas-aerosol interactions” can amplify their impact.

“We’ve known for years that methane and carbon monoxide have a warming effect,” said Drew Shindell, a climate scientist at the NASA Goddard Institute for Space Studies (GISS) in New York and lead author of a study published this week in Science. “But our new findings suggest these gases have a significantly more powerful warming impact than previously thought.”

Mixing a chemical soup

When vehicles, factories, landfills, and livestock emit methane and carbon monoxide into the atmosphere, they are doing more than just increasing their atmospheric concentrations. The release of these gases also have indirect effects on a variety of other atmospheric constituents, including reducing the production of particles called aerosols that can influence both the climate and the air quality. These two gases, as well as others, are part of a complicated cascade of chemical reactions that features competition with aerosols for highly reactive molecules that cleanse the air of pollutants.

Aerosols can have either a warming or cooling effect, depending on their composition, but the two aerosol types that Shindell modeled -- sulfates and nitrates -- scatter incoming light and affect clouds in ways that cool Earth. They are also related to the formation of acid rain and can cause respiratory distress and other health problems for those who breathe them.

Human activity is a major source of sulfate aerosols, but smokestacks don’t emit sulfate particles directly. Rather, coal power production and other industrial processes release sulfur dioxide -- the same gas that billows from volcanoes -- that later reacts with atmospheric molecules called hydroxyl radicals to produce sulfates as a byproduct. Hydroxyl is so reactive scientists consider it an atmospheric "detergent" or "scrubber" because it cleanses the atmosphere of many types of pollution.

In the chemical soup of the lower atmosphere, however, sulfur dioxide isn’t the only substance interacting with hydroxyl. Similar reactions influence the creation of nitrate aerosols. And hydroxyls drive long chains of reactions involving other common gases, including ozone.

Methane and carbon monoxide use up hydroxyl that would otherwise produce sulfate, thereby reducing the concentration of sulfate aerosols. It's a seemingly minor change, but it makes a difference to the climate. “More methane means less hydroxyl, less sulfate, and more warming,” Shindell explained.

His team’s modeling experiment, one of the first to rigorously quantify the impact of gas-aerosol interactions on both climate and air quality, showed that increases in global methane emissions have caused a 26% decrease in hydroxyl and an 11% decrease in the number concentration of sulfate particles. Reducing sulfate unmasks methane’s warming by 20-40% over current estimates, but also helps reduce negative health effects from sulfate aerosols.

In comparison, the model calculated that global carbon monoxide emissions have caused a 13% reduction in hydroxyl and 9% reduction in sulfate aerosols.

Nitrogen oxides -- pollutants produced largely by power plants, trucks, and cars -- led to overall cooling when their effects on aerosol particles are included, said Nadine Unger, another coauthor on the paper and a climate scientist at GISS. That’s noteworthy because nitrogen oxides have primarily been associated with ozone formation and warming in the past.

A new approach

To determine the climate impact of particular greenhouse gases, scientists have traditionally relied on surface stations and satellites to measure the concentration of each gas in the air. Then, they have extrapolated such measurements to arrive at a global estimate.

The drawback to that "abundance-based approach," explained Gavin Schmidt, another GISS climate scientist and coauthor of the study, is that it doesn’t account for the constant interactions that occur between various atmospheric constituents. Nor is it easy to parse out whether pollutants have human or natural origins.

“You get a much more accurate picture of how human emissions are impacting the climate -- and how policy makers might effectively counteract climate change -- if you look at what’s emitted at the surface rather than what ends up in the atmosphere,” said Shindell, who used this “emissions-based” approach as the groundwork for this modeling project.

However, the abundance-based approach serves as the foundation of key international climate treaties, such as the Kyoto Protocol or the carbon dioxide cap-and-trade plans being discussed among policymakers. Such treaties underestimate the contributions of methane and carbon monoxide to global warming, Shindell said.

Unpacking the implications

According to Shindell, the new findings underscore the importance of devising multi-pronged strategies to address climate change rather than focusing exclusively on carbon dioxide. “Our calculations suggest that all the non-carbon dioxide greenhouse gases together have a net impact that rivals the warming caused by carbon dioxide."

In particular, the study reinforces the idea that proposals to reduce methane may be an easier place for policy makers to start climate change agreements. “Since we already know how to capture methane from animals, landfills, and sewage treatment plants at fairly low cost, targeting methane makes sense,” said Michael MacCracken, chief scientist for the Climate Institute in Washington, D.C.

This research also provides regulators insight into how certain pollution mitigation strategies might simultaneously affect climate and air quality. Reductions of carbon monoxide, for example, would have positive effects for both climate and the public’s health, while reducing nitrogen oxide could have a positive impact on health but a negative impact on the climate.

“The bottom line is that the chemistry of the atmosphere can get hideously complicated,” said Schmidt. “Sorting out what affects climate and what affects air quality isn’t simple, but we’re making progress.”

Related links:
› Interaction of Ozone and Sulfate in Air Pollution and Climate Change
› Science to Support a Unified Policy on Climate Change and Air Quality
› Methane’s Impact May be Twice Previous Estimates
› Aerosols and Climate Change
Adam Voiland,  NASA's Earth Science News Team

Contact:  Sarah DeWitt or Adam Voiland, NASA's Goddard Space Flight Center, (301) 286-0535 or (301) 352-4631.  sarah.l.dewitt@nasa.gov / avoiland@sesda2.com

This text derived from:  http://www.nasa.gov/topics/earth/features/aerosol_boost.html
Link: http://earthobservatory.nasa.gov/Newsroom/view.php?id=40975&src=eoa-nnews

How well is Argo able to observe global ocean changes in temperature, chemistry, sea levels?

How well is Argo able to observe global ocean changes?

A key objective of Argo is to observe ocean signals related to climate change. This includes regional and global changes in ocean temperature and heat content, salinity and freshwater content, the steric height of the sea surface in relation to total sea level, and large-scale ocean circulation.

The global Argo dataset is not yet long enough to observe global change signals. Seasonal and interannual variability dominate the present 5-year, globally averaged, time series. Sparse global sampling during 2004-2005 can lead to substantial differences in statistical analyses of ocean temperature and trend (or steric sea level and its trend, e.g., Leuliette & Miller, 2009). Analyses of decadal changes presently focus on comparison of Argo to sparse and sometimes inaccurate historical data. Argo's greatest contributions to observing the global oceans are still in the future, but its global span is clearly transforming the capability to observe climate-related changes.

Global coverage is essential, but for global change applications, Argo data must also have high accuracy and minimal systematic errors. Therefore, a high priority for Argo is to continue work aimed at identifying and correcting pressure measurement errors, especially those with systematic impacts. High quality shipboard CTD transects are critical for assessing data quality in nearby profiling floats.
Global change observations
Ocean temperature and heat content
Ocean salinity and freshwater content
Steric sea level
Ocean circulation


Ocean temperature and heat content Over the past 50 years, the oceans have absorbed more than 80% of the total heat added to the air/sea/land/cyrosphere climate system (Levitus et al., 2005). As the dominant reservoir for heat, the oceans are critical for measuring the radiation imbalance of the planet and the surface layer of the oceans plays the role of thermostat and heat source/sink for the lower atmosphere.

Domingues et al. (2008) and Levitus et al. (2009) have recently estimated the multi-decadal upper ocean heat content using best-known corrections to systematic errors in the fall rate of expendable bathythermographs (Wijffels et al., 2008). For the upper 700 m, the increase in heat content was 16 x 1022 J since 1961. This is consistent with the comparison by Roemmich and Gilson (2009) of Argo data with the global temperature time-series of Levitus et al. (2005), finding a warming of the 0 - 2000 m ocean by 0.06 °C since the (pre-XBT) early 1960s.




Ocean salinity and freshwater content Among the major societal impacts of climate change is an increase in the global cycle of evaporation and rainfall caused by a warmer ocean surface layer. Changes in the patterns and magnitude of rainfall and storms affect nearly every facet of society, from agriculture and urban water supplies to disease and health, to housing, transportation and insurance impacts of severe weather. While the impacts are local and regional, the causes and patterns are global.

Regionally, the ocean becomes fresher or saltier where the balance between evaporation minus rainfall tips in one direction or the other over time. As an integrating measurement made with high accuracy, freshwater content (salinity anomaly over a layer) is the most sensitive yardstick available for observing the global fingerprint of a changing hydrological cycle. A second application of salinity is to diagnose the global volume of ice. Melting of either floating ice or glaciers and ice sheets lowers ocean salinity.

Recent analysis of Argo data in relation to the historical record show an increase in salinity in evaporative mid-latitude regions and a freshening at high latitudes and tropical convergence zones. This pattern may imply an increase in the global hydrological cycle by several percent (Hosoda et al., 2009; Johnson & Lyman, 2008).



Steric sea level Steric sea level provides a great example of Argo's complementary relationship with other observing system elements, particularly the altimeter Jason. Argo provides the capability to understand sea level change by measuring its component due to subsurface temperature and salinity. The steric component is dominant over the mass component in regional sea level variability and on a global basis it accounts for about 1/3 of total sea level increase in the past half century (Domingues et al., 2008). Accurate projections of future sea level require an understanding of the causes of sea level change in the modern record.

On seasonal and longer time-scales, sea surface height is dominated by changes in subsurface density. Thus, by measuring temperature and salinity as a function of depth, Argo reveals not only how much of sea surface height variability is steric in origin, but also how the steric signal is distributed over depth and between temperature and salinity. Combining sea surface height measurements from the Jason altimeter and Argo's ability to see below the ocean surface, climate related basin-scale signals on interannual and decadal timescales, such as a 15-year spin-up of the South Pacific gyre described by Roemmich et al. (2007) are becoming apparent. On global scales, Argo and Jason, together with satellite gravity measurements, partition global sea level rise into its steric and mass-related components (Wunsch et al., 2007; Willis et al., 2008; Cazenave et al., 2009; Leuliette & Miller, 2009).



Ocean circulation

The oceans are not only reservoirs for heat and water in the climate system. They are dynamically active, redistributing heat and water by means of an ocean circulation that responds to changes in wind and thermohaline forcing. Argo presently observes only the interior upper-ocean circulation, so a complete observing system that includes boundary currents and deep measurements is essential for understanding the entire ocean circulation. Some recent papers describing upper-ocean circulation include Roemmich et al.'s 2007 paper on Argo contributing to estimating changes in gyre-scale circulation, Gille's 2008 paper on the Antarctic Circumpolar Current and Hernández-Guerra et al.'s 2008 paper on the Atlantic meridional overturning circulation.

Link: http://www.argo.ucsd.edu/global_change_analysis.html

Long-term mean sea level change

Long-term mean sea level change
 
from the University of Colorado at Boulder

Long-term mean sea level change is a variable of considerable interest in the studies of global climate change. The measurement of long-term changes in global mean sea level can provide an important corroboration of predictions by climate models of global warming. Long term sea level variations are primarily determined with two different methods. Over the last century, global sea level change has typically been estimated from tide gauge measurements by long-term averaging. Alternatively, satellite altimeter measurements can be combined with precisely known spacecraft orbits to provide an improved measurement of global sea level change.
 
Since August 1992 the satellite altimeters have been measuring sea level on a global basis with unprecedented accuracy. The TOPEX/POSEIDON (T/P) satellite mission provided observations of sea level change from 1992 until 2005. Mean sea levelJason-1, launched in late 2001 as the successor to T/P, continues this record by providing an estimate of global mean sea level every 10 days with an uncertainty of 3-4 mm. The latest mean sea level time series and maps of regional sea level change can be found on this site. Concurrent tide gauge calibrations are used to estimate altimeter drift. Sea level measurements for specific locations can be obtained from our Interactive Wizard. Details on how these results are computed can be found in the documentation and the bibliography. Please contact us for further information.
 

Mass balance of the West Antarctic Ice Sheet

Mass balance of the West Antarctic Ice Sheet

Mass balance of the West Antarctic Ice Sheet (map/graphic/illustration)

Click here, or on the graphic, for full resolution.
Mass balance of the West Antarctic Ice Sheet. Increase in mass loss by the West Antarctic ice sheet. The mass loss has been steadily increasing since the 1970s as a result of accelerations in glacier flow; snowfall has not changed significantly in Antarctica over the past 50 years.
Sources Rignot E. et al. 2008b. Rignot, E. 2008.
Cartographer/
Designer
Riccardo Pravettoni, UNEP/GRID-Arendal
Appears in WWF Arctic Feedbacks Report
Published 2009
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