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Archive for January, 2010

Wind power grows 39% for the year

Friday, January 29th, 2010

Despite the economy, wind power in the US grew 39% in 2009, thanks mostly to the stimulus. The industry added 9,900 megawatts, about equal to natural gas, bringing wind’s total to 2%, or 9.7 million homes. Wind and gas made up 80% of new capacity. But the US lags Europe, and the pace could slow.

Less water vapor may slow warming trends

Friday, January 29th, 2010

Carbon dioxide and methane are greenhouse gases (GHGs) that trap heat in the atmosphere, warming the climate. Water vapor is a GHG too. A new study reports that water vapor in the stratosphere has decreased in the last 10 years, slowing Earth’s warming by about 25%. Yet the Earth is still warming.

The case for a climate bill

Thursday, January 28th, 2010

The New York TImes laid out The Case for a Climate Bill in a Jan. 24 editorial, disputing claims that health care will exhaust the Senate, and that the nation can’t afford higher energy prices. The Times’ reasons to pass a Climate Bill: urgency, the race for markets, and credibility. It urges: price carbon!

Past decade warmest on record, NASA data shows

Wednesday, January 27th, 2010

Data released by NASA shows that the decade ending in 2009 was the warmest on record, and 2009 was the second warmest year since 1880. The warmest year was 2005; others in the top ten are all since 1998. The temperature trend is up 0.36 degrees F per decade over 30 years, and 1.5 degrees since 1880.

Sites to refuel electric cars gain a big dose of funds

Monday, January 25th, 2010

Where do you fill up an electric car? Today, almost nowhere. However, that could change if start-up Better Place succeeds in creating a network of “charge spots.” The company just raised $350 million in venture capital for refueling sites and R&D. It will debut in Israel and Denmark in 2011.

A Pacific Island challenge to European air pollution

Tuesday, January 19th, 2010

In a first, Micronesia is taking the Czech Republic to court to challenge a planned refit of a large coal-fired power plant. It wants the plant closed to halt the plant’s emissions of greenhouse gases that Micronesia claims threaten its existence. Greenpeace is supporting Micronesia’s complaint.

Feeling that cold? Here’s why.

Friday, January 15th, 2010

As you shiver through one of the coldest and windiest winters in years, both in the US and Europe, you might think that global warming has ended. It hasn’t. What’s happening is an Arctic oscillation, in which a massive high pressure system over Greenland deflects cold air farther south than usual.

Europe’s post-Copenhagen view of Obama

Wednesday, January 13th, 2010

This Copenhagen analysis by Steven Hill of the New America Foundation in the New York Times casts the US and President Obama as the chief obstacles to progress. Obama can’t deliver because of Senate opposition. Developing countries were justified to resist. For Europe to lead, it needs more effort from the US.

ClimateYou Update

Tuesday, January 12th, 2010

Do you visit ClimateYou, want to respond/comment, but are unsure how to do it?  Visit our homepage, www.climateyou.org and click on share.  Instructions on how to post comments on the blog can be found there.  We look forward to hearing your thoughts on climate change!

Beyond Hades

Tuesday, January 12th, 2010

Some scientists are asking what the Earth’s climate was like before it became the Earth.  Don’t laugh; they may seem to have too much time on their hands, but believe me, they’re serious.  The Earth formed about 4.6 billion years ago when a cloud of gas imploded, creating dust grains and a star, which exerted gravitational attraction on nearby objects, getting larger and larger as it did, and causing more and more violent encounters, the most notable of which is the moon.  Few rocks have been found older than 3.8 billion years, which demarcates Earth’s earaliest geological eon, known as the Archaean.  Succeeding eons are called the Hadean and the Chaotian, and scientists have proposed several others:  the Nephelean, Erebrean, Hyperitian, and Titanomachean.  Why extend geological history to the pre-rock, pre-planet era?  First, having an established, agreed upon vocabulary can be useful.  Second, if the solar system is to be understood as the result of the events and processes that created it and continue to energize it, it needs a timescale that encompasses its entire history.  Similarly, to see the Earth in the cosmic context of the processes that formed and sustain it, rather than just as bits of stuff, can powerfully alter our attitudes toward it and how we treat it.