People now are saying that the IOD is the principle cause of rainfall variations over Australia, yet even apart from the increases over central-western Australia that I have tried desperately hard since 2001 to draw towards the CSIRO’s attention.
However, I recently discovered a
What irritates me no end is the failure of people at the CSIRO and Bureau of Meteorology to take the following statement about rainfall increases in central-western Australia that came to me from an e-mail by Ian Smith:
“My thinking at the moment is that the increase represents a response to the Australian continent as a whole, warming up faster than the oceans over recent time. This would increase the land-ocean temperature gradient and drive a stronger monsoon-like circulation. We have some climate model experiments, which tend to support this hypothesis.”
This may not necessarily seem to relate to the decline in rainfall over southern Australia. However, what I think – and observe from real synoptic charts – is that the “stronger monsoon-like circulation” increases the northerly component of airflow over southeastern Australia. This produces dry winds from the interior, especially in areas like southern Victoria shielded by the Great Divide, and a consequent reduction in rainfall. Why others at the CSIRO and Bureau of Meteorology fail to take this idea serious I do not know, but suspect highly political motives are involved.
2 comments:
FOR THE RECORD: It is stated above that I compiled the UNSW data referred to above and that I confirmed an element of the data to Mr Beeney. That is wrong. I am a UNSW journalist, not a scientist, and I wrote the media release about the research. Mr Benney did contact me by e-mail, and I forwarded his query to the scientists concerned.
Bob, I am really sorry that I said you compiled the research instead of merely having written the media release! I will try to be far more careful in the future - I may have misread you when checking e-mail!
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