Tag Archives: weather

Antarctic Plane Crash Kills 3 Canadians

Polar research requires ships, planes, and helicopters to supply bases and move people, instruments, fuel, and food to places where instruments need to placed, recovered, or serviced. While these activities are fairly routine and safe where most of us live, they are neither routine nor safe in extreme cold, extreme winds, or extremely remote places such as Arctic Canada, Greenland, or Antarctica.

I just learnt from an NSF Press Release that a Kenn Borek Twin Otter crashed into Mount Elizabeth in the Queen Alexandra Range of the Transantarctic Mountains at an elevation of about 3,900 m or 11,000 feet less than 2 weeks ago. All three Canadian crew aboard were killed. The plane was in transit from a research station at the South Pole to the Italian station at Terra Nova Bay to support Italian field work.

A memorial ceremony for the aircrew at NSF's Amundsen-Scott South Pole Station [Photo Credit: Blaise Kuo Tiong, NSF]

A memorial ceremony for the aircrew at NSF’s Amundsen-Scott South Pole Station [Photo Credit: Blaise Kuo Tiong, NSF]

Here are the words of Dr. Kelly Falkner, Director of NSF’s Polar Division (source):

January 28, 2013
On behalf of the U.S. National Science Foundation and all in the U. S. Antarctic Program, I wish to extend our profound sympathies to the families, friends, and colleagues of the three Kenn Borek Twin Otter crew, whose deaths in Antarctica while en route to support the Italian national Antarctic science program have recently been confirmed.

We have been privileged to experience first-hand their professionalism, skill, and dedication to the arduous task of supporting science in an extremely remote and inhospitable environment. In many ways, their contributions make possible hard won but vital advances in scientific knowledge that serve all of mankind. Although everyone associated with the pursuit of science in Antarctica makes personal sacrifices to do so, very infrequently and sadly, some make the ultimate sacrifice.

While it may come as little consolation at this very sorrowful time, the families, friends, and colleagues of the crew members should know that the thoughts of everyone in the U.S. Antarctic Program were with them through the long ordeal of the past few days and remain so now.

To the families and friends of the crew, I commend your loved ones for their commitment and dedication to their profession and offer our condolences. The sense of loss is keenly felt throughout the U.S. program and no doubt throughout the international Antarctic community.

-NSF-

I am also thinking of Marty Bergmann, a Canadian Polar scientist turned administrator. He perished 2 summers ago in a plane crash outside Resolute, Nunavut in the Canadian High Arctic working his Government Canada job to tirelessly help others in their Arctic research. Unlike the photo below, I remember him with a massive ear-to-ear grin on his face and a twinkle in his eye.

The Royal Canadian Geographic Society will recognize Martin Bergmann, the director of the Polar Continental Shelf Program who died in a plane crash in Resolute last year, by creating a medal for excellence in Arctic leadership, science and exploration. [Credit: CBC News]

Martin Bergmann, Director of the Polar Continental Shelf Program who died in a plane crash in Resolute Aug.-20, 2011. [Credit: CBC News]

Storm Surges, Global Warming, and Delaware Beaches

ADDENDUM (Nov.-7, 2012): Time lapse video from Delaware Sea Grant.

Rising seas and flood waters cause most of the damage during storms such as Sandy did last week. Tides, waves, and storms all contribute. We can debate how global warming impacts any of the above, but the arguments are involved. So lets assume, that neither tides, waves, nor storms are impacted by global warming, but that the globally averaged rise in sea level over the last 50 or 100 years is. This global warming induced sea level rise is about half a foot in 50 years (3 mm/year), but why would we care about global averages, when we live in Delaware? Furthermore, why worry about the whimpy surges we get ever 2-3 weeks. We don’t, we worry most about the most extreme events like Sandy and want to know how often they occur. Below I show a Sandy-like event to occur about once every 10 years. Furthermore, over time Delaware’s most extreme storm surges are rising twice as fast as global averages do. So, how much does the global warming impact our local flooding in Delaware?

Market Street on the beach in Lewes is in one of the lowest lying areas of town and takes its good old-time draining. This photograph looks northeastward toward the beach, just west of the intersection with Massachusetts Avenue. [Credit: Cape Gazette]

More than I initially thought: the largest storm surge that has hit Delaware was the Ash Wednesday storm on March 6, 1962 which added 5.8 feet to the regular tides and waves. I wrote about this yesterday using public NOAA data. This same storm today would add 6.8 feet to the regular tides and waves. For comparison, Sandy’s storm surge added 5.3 feet. So Sandy was a weak storm by comparison. If it had hit in 1962, it would have added only 4.3 feet. The difference of 1 foot in 50 years is due to steadily rising sea levels:

Largest storm surge at Lewes, Delaware each year from 1957 to present. The red line is a linear fit to the data. The slope indicates that the largest storm surge increase by almost 3 inches every 10 years.

On average each year has a larger largest surge than the year before. While this steady increase by 2.8 +/- 1.7 inches each 10 years is statistically significant (95% confidence), picking the extreme each year is perhaps not the best statistic as extremes do not happen often. Please note that a 95% confidence means that there is a 5% chance that the true increase is either smaller than 0.9 inches/decade or larger than 4.5 inches/decade.

What about the mean or average surge each year? From hourly data, I pick the middle surge, that is, half the surges each year are larger and half are smaller:

This increase of 1.4 +/- 0.2 inches per decade (95% confidence) is more in line of the global average. The uncertainty in this trend is smaller than that of the trend for the extreme, because the median sea level varies little from year to year, while the extreme value varies more from year to year. So, from these results we can conclude, that while the mean or median sea level at Lewes increases by perhaps 1.5 inches in 10 years, the extremes increase twice as fast. So, storm surges like Sandy will become more common than they are today mostly because of global warming.

Over the last 50 years we had at least 5 such events in 1962, 1968, 1996, 1998, and 2012. So, on average we have a Sandy-type storm surge greater than 5 feet every 10 years. This contradicts a Wilmington News Journal article today which quotes John Ramsey to describe “… Sandy as a 1-in-200-years storm, unlikely to be repeated anytime soon. That could give coastal communities time enough to deal with the real threats and realities of sea level rise and climate change.” There is no such time, as it is mis-leading to describe Sandy as a 1-in-200-year event when it has happened about every 10 years during the last 55 years. Instead of a 0.5% percent chance of a Sandy-like event to hit Lewes each year, I would raise this chance to be larger than 10%.

Rising Seas, Storms, and Flooding

Ocean waters are rising and flooding inland waters in Delaware and elsewhere. Some of this is perfectly regular and normal such as the up and down of the tides. Some of it is irregular and normal such as caused by storms, river discharges, waves, and weather. And some is caused by global warming as we continue to burn coal and oil to power our economies. Lets have a quick look at what all this looks like and try to put this into some perspective, but Sandy’s 5.3 feet surge last monday was second to the 5.5 feet surge that hit Lewes in 1962.

Cedar Street in Lewes flooded on Monday, October 29. (Photo by: Don Bland), as published by Cape Gazette.

The up and down of the tides each day is about 3 feet in Lewes, Delaware. This large change in sea level is so regular, normal, and predictable, that I remove it from all further discussion, because I want to know how extreme an event this week’s storm Sandy was. For this purpose I downloaded all the hourly tide gauge data from Lewes, Delaware from NOAA. The record starts in 1957 and is ongoing. Here is how the record looks for the last 4 weeks including the surge caused by Sandy last monday:

Sandy’s storm surge added 5.3 feet to the regular tide which is second-largest surge in the historical record. The largest surge at Lewes, DE was caused by the 1962 Ash Wednesday Storm that added 5.5 feet to the regular sea level:

So while Sandy was a very large surge, it was neither unprecedented nor a once in a century event. Furthermore, and this is where I come back to global warming, the 5.3 feet 2012 surge of Sandy includes the last 50 years of steady sea level rise which comes to about an inch every 10-15 years or about half a foot in the ~50 years between 1962 and 2012. So, a repeat of the 1962 storm system would cause a 6.0 feet and not the 5.5 feet surge that took place in 1962.

Furthermore, while the real size of the surge depends on where the center of the storm makes land-fall or where you are relative to the storm, the rising seas caused by global warming are much more uniform, that is, they are little different in Boston, New York, Lewes, Norfolk, or even San Francisco:

So, global warming and the rising seas it causes are both real and here to stay. Global warming provides the upward creeping background sea level to which larger tides, waves, and surges add. The combined effect of all these cause the coastal flooding. So 50 years from now, a rare, but perhaps perfectly natural freak storm like Sandy will cause a storm surge of 5.8 instead 5.3 feet on account of global warming. About 1/3 of this added sea level is caused by the oceans expanding as they warm, another 1/3 is caused by melting glaciers and ice sheets in Greenland and Antarctica, and the last 1/3 is caused by other processes. So, what happens on Greenland or China does not stay there, it impacts present and future sea level in Lewes, DE.

Hurricane Sandy, Global Warming, and the Butterfly Effect

I am stupid. I do not believe in Global Warming. No need to believe in what you know. And I know that globally averaged air temperatures increased for the last 150 years or so. I did the math myself using observations to conclude, that air temperatures around northern Greenland and Ellesmere Island increased 5 times the global average over the last 25 years (Greenland’s Warming, Melting, and Sliding to Sea). So, why am I stupid?

Cover of Bloomberg Businessweek, Nov.-5, 2012

I am stupid, because I totally disagree with what has just hit the news stand about Hurricane Sandy’s impact on the eastern seaboard of North America: It’s Global Warming, Stupid screams this week’s edition of Bloomberg Businessweek with a dramatic cover draped in red.

I do not deny that some element of global warming scenarios contributed in some way to this storm, but so did the butterfly I rescued earlier this year from my cat Zoe. The butterfly flapping her wings, I am convinced, contributed to the atmospheric turbulence and thus the weather we got, including Sandy. If this sounds crazy, it is, but so is the headline. We can argue all day, if Global Warming or my Butterfly Effect contributed more significantly to Sandy, but we will not come to a firm scientific conclusion.

The Businessweek article has some excellent points on page three with regard to climate change and policies that we can and should make to reduce carbon emissions, but it discredits these well-reasoned policies by using flood waters in Manhattan as the call for action with a screaming headline calling me stupid. If we make policies based on ill-informed drama, political manipulations, and without supporting good empirical evidence, then we do harm.

A shallow and short-term political victory does not address the deep and long-term social problems posed by climate change. Solutions to these problems such as carbon-trading, energy efficiency, smart growth, and adaptations are all endangered, if we chose to exploit emotions of the moment. This sets us up for an equally ill-informed and short-sighted political backlash. We ignore science at our own peril. This cuts both ways with regard to the political hackery and partisan politics on the issue of climate change. I can’t stand it, but then, I am stupid.

ADDENDUM Nov.-2: An excellent description of the storm’s evolution and relation to climate was published in Science Magazine.

Arctic Sea Ice Cover and Extreme Weather Explained

Addendum Sept.-24, 2012: A New Climate State, Arctic Sea Ice 2012 (video by Peter Sinclair).

I just discovered an outstanding interview that Dr. Jennifer Francis of Rutgers University gave to a non-profit community radio station out of Vancouver, British Columbia.

Jennifer Francis Interview 20120910

She connects and explains global warming, its much amplified signal in the Arctic, the extreme record minimal Arctic sea ice cover this summer, and how the warming Arctic and its disappearing sea ice impacts our weather in the northern hemisphere by slowing down the atmospheric jet stream separating polar from mid-latitude air masses. She explains all of this in non-technical language without loss of accuracy.

Dr. Jennifer Francis, Rutgers University [Photo Credit: ARCUS]

If this program piques your interest and you want to read more, Andrew Revkin of the New York time has led an informed discussion at his New York Times blog Dot Earth. And finally, Climate Central presented and illustrated Dr. Francis’ observations and ideas rather well with graphics and videos.

Nares Strait 2012: Weather Stations and Polar Bears

Weather stations offer basic information that relate to the motion of air, ice, and water. As part of our Nares Strait experiments and expeditions that started in 2003, a group of Canadian, Danish, English, Scottish, and US scientists began installations of a small network of such stations. The first and perhaps most prominent was placed on Hans Island which was a joint Danish and Canadian operation with the data hosted in real-time by the Scottish Association of Marine Science (SAMS, they also host data from Littleton Island on Greenland). This station was refurbished about 10 days ago from the Canadian Coast Guard Henry Larsen:

Dave Riedel (kneeling) and Don Dobbin (standing) on Hans Island during routine maintenance of the weather station. View is across Nares Strait with Ellesmere Island, Canada is towards the north-west. [Photo Credit: Allison Einolf, University of Delaware summer undergraduate intern from Macalaster College.]

Another weather station was placed last week by Dave Riedel and Ron Lindsay with the helicopter pilot Don Dobbin on Brevoort Island, Canada. Dave, who is shown above at the Hans Island weather station just posted his account and close encounters with two polar bears at the University of Oxford’s Arctic Ocean Research page. As a teaser I show the island as seen from the helicopter. Can you find and see the two polar bear in this photograph?

Bears on Brevoort Island, Ellesmere Island during the installation of an automated weather station on Aug.-13, 2012. Photo credit: Dave Riedel, British Columbia as posted at University of Oxford’s Arctic Ocean Research.

The data from the two “new” weather stations at Brevoort Island, Canada at the entrance to Alexandra Fjord and Joe Island, Greenland at the entrance to Petermann Fjord have real-time satellite data download capabilities, but these will need to be turned on from British Columbia by David Riedel and Canadian colleagues. I am not sure if they made it home when we parted yesterday night at Ottawa International Airport when they still had to make 2 or 3 connections to get home after being in the air or in transit for 3 days. More on the fun and adventure of traveling in the far north is reported by Dr. Renske Gelderloos in her blog post today at the Oxford site also. I suspect, that she wrote while being stranded somewhere between Ottawa and London.

Nares Strait 2012: A Bird’s Eye View of Nares Strait

Allison Einolf, Aug.-7, 2012

I know next to nothing about helicopters. They’ve always seemed exciting, but I couldn’t tell you anything about make or model or what makes one helicopter better than the next. As it turns out, helicopters are just as exciting as they seem on television.

Sunday morning, as our group of eight scientists met to discuss the plan for the day, Brian, the Chief Officer, interrupted to ask if anyone wanted to tag along on the first helicopter ride of the trip. Renske’s hand immediately shot up into the air, and I volunteered a little more slowly. We quickly wrapped up our meeting, and Renske and I layered on jackets and headed up to the flight deck.

Allison Einolf getting ready for an ice recon flight on the flight deck of the CCGS Henry Larsen. [Photo Credit: Jo Poole, British COlumbia]

The purpose of the flight was to give the Ice Services Specialist, Erin, a chance to look ahead at the ice cover up to Hans Island, where we were headed. She was going to make a chart of the ice to help guide the ship through the path of least resistance, and maybe do a little sightseeing. An air of excitement filled the helicopter because neither she nor the pilot, Don, had ever been up here in Nares Strait either.

Once the first bit of work was done, we flew over to Ellesmere Island to see the amazing folded ranges. The colors there are amazing – bright reds and yellows in layers, crunched up in beautiful synclines and anticlines. The hills are scored with avalanche chutes and based with alluvial fans. There are glaciers nested in the folds of the mountains, and it is simply breathtaking.

There is a stark contrast between Greenland and Ellesmere Island on either side of the Kennedy Channel. I was awestruck by Greenland while we were in Thule, but Ellesmere Island makes the Greenland side of the strait look dull and gray in comparison. It’s one of the first things you notice up here, and many members of the crew point it out on sunny days. The contrast brings up all sorts of questions about the rocks even for the casual observer.

A few theories have come up over the years as to what made the sides of the channel so different. Some think that the channel lies along some sort of fault or plate boundary, and some argue that plate tectonics has nothing to do with it. No matter how I look at it, something has to have been vastly different on each side of the strait because the Greenland side has all of these horizontal layers in a much grayer rock, and the Ellesmere side is more than just colorful layers – they bend and contort in violent and beautiful ways that seem much more active than the Greenland layers.

Both sides of the Nares Strait are beautiful in their own ways, and the view from a helicopter was spectacular. We were able to land on Hans Island, which is a great example of the carbonate rock of Greenland, and is apparently rife with marine fossils. We also flew over Franklin Island and farther south to Rawlings Bay and Jolliffe Glacier. It was the first time I had seen a large glacier close up, and it was amazing to see the ridges in the ice, and I was surprised by how much a glacier seems to look and act like a very slow moving river.

CCGS Henry Larsen as seen from atop Hans Island. The view is to the west with Ellesmere Island in the background. [Photo Credit: Allison Einolf, University of Delaware undergraduate intern]

As we flew into the fjord, I was continually amazed by how nearly vertical some of the layers of the rock were, and by the bright reds and yellows of the rock. Flying back to the ship we flew over the mountains and I was amazed by the way the rock beneath us dropped away completely as we flew into Nares Strait. The geology, the ice, and the experience of being in a helicopter were all so incredible.

Record Warming and Melting of Greenland

These are admittedly daily data, and yes, it is warm in summer everywhere, and yes, when it is warm, snow and ice melt at the surface. Here is the latest image of Greenland’s warming and melting that I lifted (figure and caption) straight from today’s NASA release:

Extent of surface melt over Greenland’s ice sheet on July 8, 2012 (left) and July 12, 2012 (right). Measurements from three satellites showed that on July 8, about 40 percent of the ice sheet had undergone thawing at or near the surface. In just a few days, the melting had dramatically accelerated and an estimated 97 percent of the ice sheet surface had thawed by July 12. In the image, the areas classified as “probable melt” (light pink) correspond to those sites where at least one satellite detected surface melting. The areas classified as “melt” (dark pink) correspond to sites where two or three satellites detected surface melting. Image credit: Jesse Allen, NASA Earth Observatory and Nicolo E. DiGirolamo, SSAI and Cryospheric Sciences Laboratory


Continue reading

Uncertainty in the Physics and Philosophy of Climate Change

I wrote this post last year for the National Journal, but it also relates to the way I think about Petermann Glacier’s ice islands. There are now at least 4 larger ice islands that formed from last year’s single calving: one is the tourist attraction off Labrador and Newfoundland, a second has left Petermann Fjord last week, a third was grounded off Ellesmere Island for much of the year and is now where #1 was Nov.-2010, while the fourth … I do not know. Last I heart, it was grounded off central Baffin Island. With this much variation of where pieces of the ice island went, how can we possibly claim any skill in predicting anything?

Petermann Ice Island PII-A on June-8, 2011 off Labrador. [Photo by Jay Barthelotte, Department of Fisheries and Oceans, Government Canada


Neither climate nor weather is linear, but this neither makes them unpredictable nor chaotic. The simple harmonic pendulum is the essence of a linear system with clear cause and effect relations. Oscillations are predictable as long as the initial forcing is small. Furthermore, a linear trend will show the pendulum to slow down due to friction. Corrections are straightforward.

Unfortunately, climate is not a simple, harmonic, or linear system. While this does not make it unpredictable or chaotic, it means that our “common sense” and loose talk of “totality of events” can easily fool us. We know that CO2 emissions for the last 150 years changed global temperatures. We also know that our current climate system has been very stable over the last 10,000 years. What we do not yet know is how small or how large a perturbations the last 150 years have been. If the pendulum is forced too much, if the spring is stretched too far, the system will find another stable state by breaking. Climate dynamics can find an adjustment less tuned to the areas where people presently live. This is what “tipping points” are about. Only numerical experimentation with the best physics and models will suggest how close to a different stable climate state we are. The IPCC process is one way to do so.

Ice cores from Greenland contain air bubbles 100,000 years old, which clearly demonstrate that our present climate state is the “anomaly of quiet” in terms of temperature fluctuations. The absence of large fluctuations for about 10,000 years made agriculture and advanced civilizations possible. The ice cores show that abrupt climate change has happened and may happen again, not this election cycle, but it is one possibility perhaps as likely as the possibility that climate change is mundane, linear, and follows trends that we can easily correct or mitigate later. Both are excellent hypotheses.

For scientists, these are exciting times as we conduct a massive, global experiment to see how much CO2 we can add to the atmosphere to perhaps find a different climate state. Dr. Terry Joyce, Senior Scientist at Woods Hole Oceanographic Institution once said: “I’m in the dark as to how close to an edge or transition to a new ocean and climate regime we might be. But I know which way we are walking. We are walking toward the cliff.” I agree with this sentiment, but add that we do not know if this cliff is a 1000 feet fall or a 2 feet step. Can we affort to wait until we know for sure? As a scientist I do not care. As a citizen, however, I think the time to act responsibly is now.

Is Climate Change Causing Wild Weather?

Almost a year ago, Amy Calder of the National Journal asked:

Are extreme weather events, when considered collectively, evidence that climate change is occurring? If not, what are the missing links scientists still need to study in order to make a more conclusive find? Could these weather events revive congressional efforts to pass comprehensive climate legislation?

My answer is still the same, even though I grapple with what my resonsibilities and moral obligations are as a scientist learning, a tenured professor teaching, and a citizen voting. Here it is:

No, climate does not cause weather, the balances of forces, masses, and energies in the atmosphere do. Furthermore, the atmosphere interacts with oceans, ice sheets, lands, and livings things. Ask an equally ill-posed question “Is climate change contributing to wild weather?” and my answer becomes yes, but with the caveat that butterflies flapping their wings in Tokyo contribute as well. There is more to the question than meets the eye.

Globally averaged air temperatures have increased by about 0.6 degrees Celsius per decade over the last 50 years. This warming is not uniform as it varies in both space and time. Some places cool, some places warm, some places cool or warm more than expected. Floods, droughts, mudslides, and calving glaciers always have and always will occur. Some weather events separated in space and time are physically linked via large-scale tele-connections such as Rossby waves in the atmospheric jet stream or the El Nino-Southern Oscillations.

So, how much of the currently observed extreme weather events are due to globally increasing air temperatures that also coincide with globally increasing ocean temperatures? Does global warming increase, say, the intensity of hurricane by 1% or 10% or 50%? These much tougher questions are at the forefront of both observational and computational work on environmental physics. The IPCC numerical models and new understanding of key physical processes, I feel, are the only way to attribute global warming effects on extreme weather events. Ice-ocean interactions around Greenland are one such physical process poorly incorporated in IPCC models. Another such process is the way that hurricanes may dominate the ocean heat flux towards Greenland.

Three weeks before Katrina hit New Orleans in 2005 MIT professor Dr. Kerry Emanuel published that the power dissipation by hurricanes has increased by about 60% over the last 30 years and that this increase correlates with increasing sea surface temperatures in the tropical North Atlantic. Nevertheless, Dr. Emanuel himself stressed that nothing could be more absurd than stating that Katrina was caused by global warming. Furthermore, refining his methodology in 2008, he finds that “… global warming should reduce the global frequency of hurricanes, though their intensity may increase in some locations.” [Emanuel et al., 2008: Hurricanes and global warming, Bull. Amer. Meteor. Soc. 89, 347-367.]

Just because a pattern of extreme weather events feels like evidence of global warming, it does not make it so. This scientific uncertainty, however, should not distract from the potential costs that a potentially man-made climate change will cause. Climate zones may shift, sea level may rise, volatile weather events may become more volatile, etc. All of this may cause additional political instabilities in marginally stable nation states ill-equipped to deal with either natural or man-made disasters.