Cross-posted at: Dailykos
Recently we saw Kerry Emanuel of the Massachusetts Institute of Technology and meteorologist Tom Knutson demonstrate that global warming may indeed be making hurricanes much more powerful:
My global warming hero Rasmus helped to explain why this might be so:
But the one huge problem in my mind has consistently been that we have almost no data on hurricane intensity that it older than 150 years. Now we do:
What we really need to know is: is this new data suggesting something that is outside the historical trend. Are we seeing something new? Hurricane activity varies greatly from year to year and from decade to decade and tells us very little about long-term trends. We can only begin to see new trends by comparing present data with historical and pre-historic trends. But the data goes back not more than 150 years and in some cases, most cases, not even that long.
Sounds like that’s going to change. Live Science reports that Claudia Mora of the University of Tennessee has devised a way to measure the intensity of a hurricane season by looking at tree rings in the southeastern pine forests.
“We’ve taken it back 100 years and didn’t miss a storm,” she said.
In my former life, I was an archaeologist and I still LOVE this stuff!
We’ve known for a very long time that one can, essentially, see the weather from ancient times by looking at tree rings. A tree ring (and associated isotopes and chemical signatures) can tell you if it was a wet or dry year, if there was a high occurrence of lightening, if there was a forest fire, if there was a volcanic eruption and so on. Here in the southwest, our detailed knowledge of tree ring data is the best in the world. You can literally find out what the weather was like in the summer of 982AD, for example. Not so in most other parts of the world. Until now.
Mora and her group have begun looking at tree ring data to determine historical trends in hurricane intensity:
Hurricane depletes the air of oxygen-18, so a hurricane’s rain has less of it than other downpours. A shallow-rooted tree like the longleaf pine draws from a storm’s rain within a couple weeks, leaving a storm’s calling card in the new tissue.
Nerd or not, this is just cool. And important.
Additional work revealed droughts and wet years in trees going back to 1450. One storm, known as the Great Hurricane of 1780, put its John Hancock in the trees.
The trees say hurricane activity from 1580-1640 was low, which matches with what scientists expect based on other clues to the climate from that time.
“What we’re trying to do is understand frequency of hurricanes and how variable their occurrence is over the long-term,” Mora said. “We’re trying to come up with a reliable way to establish this.”
Her paper is due to be published this week.
Fascinating. For the global warming non-believers this is one more nail in the coffin. When will they get it? Thanks for the diary, recommended.
Amazing. For the non-scientist like me this looks like the kind of great idea that seems so obvious you wonder why nobody ever thought of doing it before. But maybe it had to wait for the discovery of oxygen-18?
Recommended for the timeliness with regard to the articles on Siberian peat, etc. Also good to read science that’s simplified for those of us not so inclined.
Excellent summary – recommended with pleasure.
You beat me to the punch this morning! 😉
I suspect that our planet is right on the cusp of sustaining a continuous storm. With a little more energy in the system, and reduction of destabilizing factors, we may find ourselves the proud possessors of a Great White Spot.
Jupiter has a Great Red Spot. Saturn has it’s own, less stable, Great Spot. Neptune has the Great Dark Spot.
I think it’s fairly clear that these storms are prone to occur on revolving planets — and always in latitudes similar to those where hurricanes form on Earth. The storms we get today are like the sputters of an engine that can’t quite get started. Most likely, landmasses cause enough complexity in wind and ocean currents that even more energy would not give us a constant Class 6 humming off Honduras. But hey, once we melt enough of the ice caps to drown most of the small islands and peninsulas (little things like Florida), we might find ourselves the owners of a new pupil to our cosmic eyeball.
Fantastic diary. You wouldn’t be working for the Tree Ring Research Lab at the Univ. of Arizona by any chance, would you? I took an elective class from their department and it was the greatest three months.
Global warming also has the capability to affect winter weather in certain parts of this country, although I’m not sure if that is actually happening.
Parts of upstate New York have been enduring the hottest summer recorded in the last 50 years, which means that the upcoming winter of 2005-06 is probably going to be one of the worst for lake effect snowfall in recent memory. All lake temperatures in upstate New York — including the snow-generator, Lake Ontario, no doubt — are now high enough to be affecting the fish populations.
Lake effect snow occurs in the Great Lakes, usually in the eastward lee of a lake, when the lake temperatures are warm. Ice hasn’t formed on Lake Ontario for several years, and the winter of 2003-04 saw some epic snowfall in Lake Ontario’s most suspectible snowbelt – include one storm that dumped 60 inches in 18 hours.
The beauty (or horror?) of lake effect is that storms of that magnitude that can happen in certain parts of upstate NY every day, day after day. They are not dependent on nor’easters or anything like that. It’s much more dependent on water temperature and cold fronts.
Smart people here are buying new snowblowers along with their air conditioners.
are well known for this. Buffalo especially.
The Cleveland metro area stretches some 30 miles or so around a curve in the lakeshore. Because of this and the inland topography, the west side suburbs can get a light dusting of snow while the high eastern suburbs can get a foot or more.
Lake Erie gets the warmest of all the lakes, being so shallow, especially late summer through the beginning of winter I’d guess. I once had lunch at a lakeshore restaurant and watched seven waterspouts parade half a mile or so offshore downtown Cleveland one October day.
Biggest surprise to me coming from Lake Erie to Puget Sound was the lack of moisture odor on the water, due to the cooler temperatures of the water.
That is some damn fine science.
Clever idea, established a baseline, and then proceeded to break open a vital piece of research giving a new tool for investigation.
There are some people in Europe working on a dendrochonology who could use this technique to spring the information base back to the Bronze Age and could provide some snapshots into the Neolithic.
Way Cool.