Dr. Ricky Rood's Climate Change Blog |
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| Posted by: Dr. Ricky Rood, 2:12 AM GMT on November 11, 2010 | +2 |

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I'm a professor at U Michigan and lead a course on climate change problem solving. These articles include ideas from the course. And no tuition!
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Or perhaps dead microbes which feasted on the oil spill in the GOM this year???
9398281 (2007) vs 938125 (today).
As i mentionned before, we're still in the same league with figures so close. Not yet typical of a dooms cold era predicted earlier this year or more recently following a quick start within the 80 deg. above. Recent report on the ENSO status is showing a very warm SST on most of the Atlantic, and north seas (including Hudson's Bay). So even if temps goes low, SST will delay the ice formation and it is already visible in the current stats.
From the latest ENSO status report (Nov. 15th.
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So we know Methane is a much worse (25X) GHG than is Co2. Would it have been better to burn that fuel to get Co2 or is it better to let it leak out and be turned eventually into methane? Either way my Tunnels prevent that!
I was afraid of that I didn't edit it in time! Speaking world wide levels?
Aasiaat 28 °F 59% 30.06 in Scattered Clouds NE at 22 mph 9:50 AM WGT Add to My Favorites
Angisoq 38 °F 44% 29.94 in East at 17 mph 9:00 AM WGT Add to My Favorites
Aputiteeq 28 °F 54% 30.31 in NNW at 9 mph 9:00 AM WGT Add to My Favorites
Cape Harald Moltke Add to My Favorites
Cape Tobin 5 °F 56% 30.45 in Scattered Clouds WNW at 6 mph 11:50 AM EGT Add to My Favorites
Carey Island -6 °F 60% 30.11 in West at 8 mph 8:00 AM AST Add to My Favorites
Daneborg -3 °F 43% 30.29 in North at 1 mph 9:00 AM WGT Add to My Favorites
Danmarkshavn 2 °F 24% 30.25 in NW at 14 mph 9:00 AM WGT Add to My Favorites
Hall Land -22 °F N/A% 30.08 in Clear ENE at 9 mph 6:00 AM MST Add to My Favorites
Henrik Kroeyer Holme -23 °F 53% 30.09 in Calm 9:00 AM WGT Add to My Favorites
Ikermiit 26 °F 38% 30.23 in NNW at 21 mph 9:00 AM WGT Add to My Favorites
Ikermiuarsuk 30 °F 50% 30.15 in NNW at 23 mph 9:00 AM WGT Add to My Favorites
Illoqqortoormiut 5 °F 56% 30.45 in Scattered Clouds WNW at 6 mph 11:50 AM EGT Add to My Favorites
Ilulissat 25 °F 40% 30.09 in Scattered Clouds NE at 8 mph 9:50 AM WGT Add to My Favorites
Kangerlussuaq 7 °F 79% 30.09 in Scattered Clouds ENE at 9 mph 9:50 AM WGT Add to My Favorites
Kangilinnguit Add to My Favorites
Kap Morris Jesup -1 °F 58% 29.95 in Calm 9:00 AM WGT Add to My Favorites
Kitsissorsuit 31 °F 65% 30.13 in South at 23 mph 9:00 AM WGT Add to My Favorites
Kitsissut 30 °F 55% 30.01 in Scattered Clouds East at 2 mph 9:50 AM WGT Add to My Favorites
Kulusuk 27 °F 74% 30.24 in Mostly Cloudy Variable at 1 mph 9:50 AM WGT Add to My Favorites
Maniitsoq 32 °F 51% 29.98 in Mostly Cloudy ENE at 13 mph 9:50 AM WGT Add to My Favorites
Mittarfik Nuuk 32 °F 44% 29.95 in Mostly Cloudy NE at 14 mph 10:20 AM WGT Add to My Favorites
Narsarsuaq 39 °F 26% 29.92 in Scattered Clouds ENE at 30 mph 9:50 AM WGT Add to My Favorites
Navy Operated Add to My Favorites
Nerlerit Inaat 5 °F 56% 30.45 in Scattered Clouds WNW at 6 mph 11:50 AM EGT Add to My Favorites
Nunarsuit 34 °F 60% 29.94 in East at 18 mph 9:00 AM WGT Add to My Favorites
Nuuk 32 °F 44% 29.95 in Mostly Cloudy NE at 14 mph 10:20 AM WGT Add to My Favorites
Nuussuaataa 25 °F 64% 30.12 in Mostly Cloudy SE at 12 mph 9:50 AM WGT Add to My Favorites
Paamiut 33 °F 23% 29.92 in Partly Cloudy SE at 5 mph 9:00 AM WGT Add to My Favorites
Pituffik -11 °F 77% 30.12 in Scattered Clouds East at 10 mph 9:32 AM AST Add to My Favorites
Prins Christian Sund 35 °F 28% 30.08 in Mostly Cloudy WSW at 24 mph 9:00 AM WGT Add to My Favorites
Qaanaaq Add to My Favorites
Qaarsut 25 °F 64% 30.12 in Mostly Cloudy SE at 12 mph 9:50 AM WGT Add to My Favorites
Qaqortoq 39 °F 26% 29.92 in Scattered Clouds ENE at 30 mph 9:50 AM WGT Add to My Favorites
Sioralik 32 °F 51% 29.98 in Mostly Cloudy ENE at 13 mph 9:50 AM WGT Add to My Favorites
Sisimiut 30 °F 55% 30.01 in Scattered Clouds East at 2 mph 9:50 AM WGT Add to My Favorites
Sisimiut Mittarfia 30 °F 55% 30.01 in Scattered Clouds East at 2 mph 9:50 AM WGT Add to My Favorites
Station Nord Add to My Favorites
Station Nord 2 °F 41% 30.00 in SSW at 23 mph 9:00 AM WGT Add to My Favorites
Summit -48 °F 67% in Calm 9:00 AM WGT Add to My Favorites
Tasiilaq 29.3 °F 67% 30.23 in Mostly Cloudy West at 1.0 mph 10:45 AM WGT Add to My Favorites
Ukiivik 34 °F 38% 29.94 in ENE at 10 mph 9:00 AM WGT Add to My Favorites
Upernavik 30 °F 75% 30.12 in Mostly Cloudy ESE at 18 mph 9:50 AM WGT
Correct this years uptick is huge! Ouch!
OUCH! Soon the palm trees will be growing! LOL!
How long would it take a catagory 5 hurricane (30 mile wide eye) parked in one spot over the Gulfstream to upwell enough cold water to restore the Northern Arctic Ice during the summer to pre-industrial revolution extents?
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Correct Michael!
For January/October 2010, the global combined land and ocean surface temperature was 0.63C (1.13F) above the 20th century average of 14.1C (57.4F) and tied with 1998 as the warmest January/October period on record.
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"What we have seen is a rather pronounced reduction in the extent of sea ice. At the end of summer now we have 40 percent less sea ice than we had say during the 1970s," Serreze said.
"We are losing that insulator so what we are seeing now are big fluxes in heat from the ocean to the atmosphere," he said.
"Since everything is connected together in the climate system what happens up there can influence what happens down here and I am talking about in the middle latitudes."
The other thing that the scientists said is changing, along with climate, is how they confront skeptics who question the reality of climate change and the extent of humans' role in causing it.
"There are still many of us who like to sit in our office or go into the field and just do our science and not enter into the fray, but I think that is changing," said Serreze.
"We have to become more involved," he added. "We have to become better communicators. Scientists are not always good communicators of the issues but this is part of a learning curve and we have got to face that."
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But a fierce storm in the region Thursday has temperatures dropping and ice forming, which could be good news for the bears. "It's just howling," Luc Desjardins, of the Canadian Ice Service, says of the storm that could change the fortunes of the hungry bears.Until the storm hit, record-breaking conditions in the western Arctic this fall had kept the ice at bay. Temperatures up to 14 C above normal in one Arctic region in November prevented the formation of ice which was almost a month behind schedule as of Monday, says Desjardins. He says the ice cover was the lowest since 1971, covering just 1.5 per cent of the sea, compared to the average of 20 per cent by mid-November.
Polar bears need sea ice to hunt for seals and other marine mammals. And after slim pickings on land in the summer, they are ready to get back on the ice come fall.
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11:49 PM GMT on November 19, 2010
Warmer temperatures increase the capacity to hold water and the rains in the Midwest -- Northfield flooded in September, the Minneapolis folks were shocked by 20 inches of snow last week -- yes, snow shocked Minnesotans! -- and the rains this summer in Iowa created such fertile mosquito breeding conditions that people couldn't go out to garden -- well, this is increase in rainfall is something to noodle!
Reminds me of the same thing happening in the great lakes being so warm and causing more moisture which makes more snow.
Three decades have passed since the movie Jaws sent terrified bathers scrambling out of the ocean. But as any beach lifeguard knows, there's still nothing like a gory shark attack to stoke public hysteria and paranoia.
Two deaths in the waters off California and Mexico last week and a spate of shark-inflicted injuries to surfers off Florida's Atlantic coast have left beachgoers seeking an explanation for a sudden surge in the number of strikes.
In the first four months of this year, there were four fatal shark attacks worldwide, compared with one in the whole of 2007, according to the International Shark Attack File at the Florida Museum of Natural History in Gainesville.
'The one thing that's affecting shark attacks more than anything else is human activity,' said Dr George Burgess of Florida University, a shark expert who maintains the database. 'As the population continues to rise, so does the number of people in the water for recreation. And as long as we have an increase in human hours in the water, we will have an increase in shark bites.'
Some experts suggest that an abundance of seals has attracted high numbers of sharks, while others believe that overfishing has hit their food chain. 'I'm not saying it doesn't happen, but it's a convenient excuse,' Burgess said. Another contributory factor to the location of shark attacks could be global warming and rising sea temperatures. 'You'll find that some species will begin to appear in places they didn't in the past with some regularity,' he said.
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By suggesting there is light at the end of the global warming tunnel, Timoner has made “Cool It” a hopeful film. We just have to know where to look for the switch.
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I bet by the time we have a ice free summer North Arctic we will also have a year round ice free Hudson Bay!
Pretty sad all they need are Tunnels in the Kuroshio Current to run electric cars.
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One record low. Ouch! Tunnels can force many more! The movie "COOL IT" says we need to force many more record cooling events with geo-engineering.
Measuring fast-melting Arctic sea ice
You've probably seen pictures of stranded polar bears and heard that global warming is causing the melting of Arctic sea ice -- that is, floating ice formed from freezing ocean surface water. But you may imagine, as most people do, that this distant phenomenon is unfolding gradually over a centuries-long time frame.
Julienne Stroeve, a climate scientist at the National Snow and Ice Data Center in Boulder, Colo., has compiled detailed measurements that melt away any such misconceptions. Stroeve is closely monitoring the extent of Arctic sea ice, and her research shows that dramatic changes are occurring right now -- far faster than most experts anticipated and with enormous consequences for the whole planet, not just the Arctic region.For instance, during the warmest part of 2010, the total amount of Arctic sea ice -- the so-called "seasonal minimum" -- was the third-smallest ever recorded. The smallest and second-smallest seasonal minimums were measured in 2007 and 2008, respectively. Natural variability, including factors like cloud cover, can easily explain differences in melting from year to year, Stroeve notes. But the big news is that the smallest amounts of Arctic sea ice ever measured have all occurred in recent years. "Basically, ever since 2002, we've had one pronounced record minimum after another," she says. "The data all point to a strong warming signal."
Stroeve explains that highly reliable data on the extent of Arctic sea ice has been collected since 1978. From then until now, she has found clear evidence of a 30-year melting trend, which, she says, "cannot be easily explained away by natural variability." But her work is even more notable for its findings about the speed of the change. Over this same 30 years, a relatively brief period, Stroeve has found that some 40 percent of the region's summer (or more precisely, September) ice has melted.
The fast pace of melting is seen even more dramatically, she explains, when one considers the age of the Arctic ice. Many parts of the Arctic Ocean freeze each year during the coldest months. But only ice that lasts throughout the year gradually becomes thicker over the course of consecutive seasons. "In the 1980s, the Arctic contained roughly 386,000 square miles of ice that was determined to be at least five years old," she says. Now, "at the end of the melt season in September, only 22,000 square miles of such older, thicker ice remains." In other words, the region has already lost more than 97 percent of the thicker year-round ice that existed just three decades ago. As she explains, "all the climatic processes seem to be pushing rapidly toward a seasonally ice-free Arctic Ocean."
Stroeve says that initially she was as surprised by the data as anyone else. "I didn't think global warming was even happening in the early 1990s when I began this work," she says. Back then, some climate models were projecting that carbon emissions would lead to a pronounced warming trend at the poles. But Stroeve was always more interested in actual measurements than in climate modeling. "I think I was lured into studying the poles by the prospect of adventurous fieldwork in Greenland or the Alps," she says with a laugh.
The daughter of an aerospace engineer, Stroeve had always exhibited a strong aptitude for math and science and an adventuresome spirit. From childhood through her high school years, her dream was to be an astronaut, she says, and she might have continued on that track if she hadn't realized that her susceptibility to motion sickness was a serious impediment to working in space.
Her love of adventure continues in her work today, in which she makes regular research trips to the Arctic and Greenland to measure ice thickness and other snow and ice measurements. It might not be space travel, but Stroeve says her fieldwork has been as exciting as she could have hoped. "When I first visited Greenland, it was the most stunning landscape I had ever seen," she says.
Along with her research in the polar regions, much of the data Stroeve analyzes comes from satellites that detect passive microwave radiation. As she explains, the higher brightness of ice in the microwave part of the spectrum can be seen by satellites even through cloud cover. "In the often-cloudy polar regions, that makes it an incredibly useful tool, providing data in which we have a high degree of confidence," she says. These detailed satellite measurements of Arctic sea ice led Stroeve to shed her initial doubts about global warming. "My views changed as I studied the emerging data," she says. "With record low sea-ice extents year after year, it became clear that a significant warming trend was underway."
Looking closely at the data, Stroeve realized that a phenomenon called Arctic amplification, a form of positive feedback, is accelerating the warming trend, causing it to occur many years sooner than most climate models had projected. Arctic amplification occurs primarily because water absorbs far more heat than ice does. On average, Stroeve explains, water absorbs almost 93 percent of all the incoming solar radiation, whereas the white surface of snow-covered ice reflects about 80 percent of incoming solar radiation back into space.
As more and more of the Arctic Ocean sea ice melts over the summer months, it hastens further warming, Stroeve explains. She and her colleagues at the National Snow and Ice Data Center have measured the effect, showing that in areas where summer ice has disappeared, local autumn air temperatures have been more than 5 degrees F higher than the long-term average.
The potential of such feedbacks to cause abrupt climate change as the Arctic Ocean becomes nearly ice-free in the warm season drew widespread attention to Stroeve's work in 2007. In that record-breaking warm year, the Arctic Ocean lost more than one-quarter of its remaining ice. "Because new ice can't get very thick in one season, it is more vulnerable to annual temperature changes, as we saw in 2007," she says.
The possibility of sudden shifts in the region's climate, and thus the planet's climate, is the most frightening implication of her research, Stroeve says. The quick and volatile changes in Arctic sea ice remind us that the geological record contains clear evidence of abrupt climatic changes in the planet's history. "We know that Arctic ice has historically helped keep the Northern Hemisphere cool," Stroeve says. "Without it, given atmospheric circulation, the planet will certainly warm more quickly. But we don't know enough about the system to fully project how swift the changes might turn out to be."
The prospect of sudden climate change is certainly scary, Stroeve says. But she adds that, because the stakes are so high, her decision to study Arctic sea ice has proven a more exciting choice than she ever imagined. As she puts it, "Not a lot of people were looking at sea ice when I began my research. But especially after 2007, which took everyone by surprise, it has become something that climate scientists are intensely interested to know about."
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Could that be from tropopause folds? There was some banter about concerning one of the typhoons causing a significant event...cannot remember which or when, exactly...
A new study finds that the warm Atlantic Ocean current known as the Gulf Stream could influence the climate of remote regions by pumping heat high into the atmosphere above it. The powerful current, which flows up from the Gulf of Mexico along the U.S. east coast and across the Atlantic to western Europe, is known to influence the formation of cyclones and clouds as well as to moderate the climates of the regions it touches. But Japanese researchers wondered if it had further-reaching effects. Combining high-resolution satellite data with water analyses, they discovered a pattern of airflow that reaches seven miles (10 kilometers) high, well into the upper part of the troposphere, the lowest and most massive layer of Earth's atmosphere. Winds blow toward the warm Gulf Stream from the colder waters on its western edge, causing a warm updraft and a consequent narrow rainy region along the current. The upward airflow (depicted in this image as vertical streaks) generates clouds in the upper troposphere that branch out and travel toward Europe. Reporting in Nature, the researchers note that this pattern suggests a way that the Gulf Stream might influence both local and distant climates good to know in case global warming hits the brakes on the current as it is expected to do.
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UPWELLING
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Upwelling is an oceanographic phenomenon that involves wind-driven motion of dense, cooler, and usually nutrient-rich water towards the ocean surface, replacing the warmer, usually nutrient-depleted surface water. The increased availability in upwelling regions results in high levels of primary productivity and thus fishery production. Approximately 25% of the total global marine fish catches come from five upwellings that occupy only 5% of the total ocean area. [1] Upwellings that are driven by coastal currents or diverging open ocean have the greatest impact on nutrient enriched waters and global fishery yields. [1] [2]Types
Upwelling animated.gif
Upwelling near the coast due to Ekman transport perpendicular to the wind in the northern hemisphere.
The major upwellings in the ocean are associated with the divergence of currents that bring deeper, colder, nutrient rich waters to the surface. There are at least five types of upwelling: coastal upwelling, large-scale wind-driven upwelling in the ocean interior, upwelling associated with eddies, topographically-associated upwelling, and broad-diffusive upwelling in the ocean interior.Other sources
* Local and intermittent upwellings may occur when offshore islands, ridges, or seamounts cause a deflection of deep currents, providing a nutrient rich area in otherwise low productivity ocean areas. Examples include upwellings around the Galapagos Islands and the Seychelles Islands, which have major pelagic fisheries. [1]
* Upwelling can also occur when a tropical cyclone transits an area, usually when moving at speeds of less than 5 mph (8 km/h). The churning of a cyclone eventually draws up cooler water from lower layers of the ocean. This causes the cyclone to weaken.
* Artificial upwelling is produced by devices that use ocean wave energy or ocean thermal energy conversion to pump water to the surface. Ocean wind turbines are also known to produce upwellings. [4] Ocean wave devices have been shown to produce plankton blooms. [5]
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"TUNNEL UPWELLING"
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