I have closed several comment threads which were the recipients of the bulk of recent "spam" comments - it's pretty annoying weeding through all that stuff, so hopefully this will simplify my life a little.
Almost 6 years ago, in September 2004, I was intrigued by the Toyota Prius and put myself on one of the waiting lists for a car. Somewhat unexpectedly they actually had a car for me by April 2005. It was a delight from the moment I first test-drove it, and the only car I've liked more in the time since has been a 2010 Prius I was a passenger in earlier this year. It wasn't just the fancy hybrid electric drive, nor being able to ride in the expressway HOV lane any time I want, joyful as those things might be. Somehow the car expresses a compact perfection that's hard to put into words. The interior is spacious, the seats comfortable, the controls (dashboard and all over the steering wheel) easy to reach and intuitive. The digital speedometer and other urgent indicators above the main dashboard give a different feel from other cars I've been in, one that emphasizes what's important, and lets you ignore the irrelevant. The keyless entry and push-button ignition (thanks to an RFID key that never leaves my pocket) spoil me for other cars I have to drive on occasion.
But the meat of the car is the hybrid engine and fuel efficiency. So how does that do? The dashboard monitor tells me how I'm doing, usually somewhere between 40 and 50 miles per gallon. But I wanted to keep better track, so after my first year I decided to start recording my gas purchases; the following graph shows the record:
[The following is in regard to models of the high temperature of the surface of Venus which ascribe that high temperature essentially to the high atmospheric pressure on that planet, without properly recognizing the role of infrared absorption by greenhouse gases. In particular, Leonard Weinstein, in previous discussions there, had essentially claimed that even if all solar radiation were absorbed by a thin high layer in Venus' atmosphere at a relatively cool temperature, the surface temperature would still be very high. The following is why I disagree.]
Keith Kloor is a free-lance writer who reportedly now teaches journalism at NYU; during 2008-2009 he was on some sort of fellowship in Colorado. He has been blogging for a couple of years on climate issues at Collide-A-Scape, generally on meta-level issues concerning the image of particular individuals and their claims in discussions of climate, rather than any technical science questions. Some of his stuff has been mildly interesting. His best stuff has been interviews with bloggers and scientists who have had differing stances in discussions.
Dr. Judith Curry is chair of the School of Earth and Atmospheric Sciences at Georgia Tech, and has an extensive background in studying Earth's climate, particularly regarding changes in storms, hurricanes, and the like under changing climate conditions. She recently coauthored what seems a very interesting paper on the growth of Antarctic sea ice - apparently the effect of a moderate degree of warming such as we've seen so far is to actually increase sea ice extent in the southern ocean, thanks to increased precipitation in the form of snow. Higher sea temperatures mean more evaporation of water (mostly closer to the equator) which in turn leads to higher levels of precipitation (mostly further south), and if it's cold enough to snow, then paradoxically the result is actually more ice on the water surface, not less.