The Great Moral Challenge, but Kevin Rudd now thinks its a challenge that can be put off for a few years. Kevin Rudd who said we had to have the ETS (Emissions Trading Scheme) in place before Copenhagen December 2009, to set an example to the world. We would loose the Great Barrier Reef if we did not have an ETS.
Now its not so desperate?
That would not be because Climate Change Skepticism is on the rise would it Kevin?
If Kevin Rudd really believed this, he would go to a double dissolution Election and fight his case, and get the ETS bill passed as a joint sitting of the House of Reps and the Senate after the election (if he won).
The real reason is that Kevin Rudd and the Labor party have embraced Climate Change is that it is a trendy political cause, and that cause has lost its popularity. We don’t here the “Global warming the end is nigh” stories every day, because even the naive journalists have realised its more religion than science.
And what about the Greens? Political purity is more important than practice? They want to reduce Carbon emissions, they block the bill because its not “pure” enough for them, and they end up with no bill, no scheme to reduce carbon at all. What were they thinking?


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[...] Factors that can shape climate are climate forcings. These include such methods as variations in solar radiation, deviations in the Earth’s orbit, mountain-building and continental drift, and changes in greenhouse gas concentrations. There are a selection of climate change feedbacks that can either strengthen or make smaller the initial forcing. Some sections of the climate system, such as the seas and ice caps, respond bit by bit in response to climate forcing because of their large mass. Therefore, the climate system can take many many years or longer to entirely respond to new external forcings. Australian blog on Climate Change [...]
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[...] the climate system can take centuries or more to completely respond to new external forcings. Australian blog on Climate Change Read [...]
[...] Factors that can have an effect on climate are climate forcings. These include such systems as alterations in incoming solar radiation, alterations in the Earth’s orbit, mountain-building and continental drift, and changes in carbon dioxide and other greenhouse gas concentrations. There are a variety of climate change feedbacks that can either amplify or diminish the initial forcing. Areas of the atmosphere, such as the oceans and ice caps, react slowly in reply to climate forcing because of their large mass. Therefore, the climate system can take hundreds of years or longer to completely react to new external forcings. australian climate change [...]