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Did you know?" column on
December 10, 2006. The text of the entry was: Did you know ...that coral within tropical oceans is being used as a
tropical cyclone observation to date past hurricanes, by looking for concentrations of the oxygen isotope
O-18? | ||||||||||||
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What was the unheralded typhoon in WWII that upset sea battle plans? It should get a passing mention in the opening. -- Wetman 22:57, 10 December 2006 (UTC)
This article has passed the GA noms. The following are bot-generated suggestions for improvment.
The following suggestions were generated by a semi-automatic javascript program, and might not be applicable for the article in question.
You may wish to browse through User:AndyZ/Suggestions for further ideas. Thanks, Tarret 14:26, 17 March 2007 (UTC)
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BetacommandBot 02:29, 6 September 2007 (UTC)
I would like to see the observation techniques organized more logically into larger groups like:
1. Remote sensing techniques: satellite, radar, lightning detection, (GPS meteorology)
2. Upper air/ In situ measurements, like aircraft observations, radio sounding, drop soundings, drifters, rocket sounding
3. Surface observations: a) fixed stations/platforms: weather / coastal/ island observation stations, tidal stations (water level), buoys, drilling etc. platforms; b) moving platforms: ships,
drifting buoys
4. Sub-surface observations: some operational marine observation methods which are useful and used in detecting regions favorable for hurricane generation/ dissipation
5. Historical/Geological evidence: this could include the non-real time methods written already
What do you think, should we proceed and reorganize this article and add a few new techniques now missing?
-- Paju ( talk) 23:21, 20 November 2007 (UTC)
-- Thanks for your response. I agree: Starting with surface observations - which everybody can feel and verify themselves on the ground in case of tropical cyclone is occurring - might be the most (?) logical starting point. Historical documents like log books etc (e.g. original of Beaufort scale including the definition of "hurricane force" wind was originally written on a log book - of which I have a copy from the Royal Society; similar stuff is available by many other great historical figures of meteorology as well) could be another starting point. Third option is the remote sensed data (of tropical disturbance) which is nowadays quite often the real starting point for forecasts of tropical cyclone development. But let us see what I can make up... :c) -- Paju ( talk) 20:24, 22 November 2007 (UTC)
Cast your votes for:
I propose holding the voting open for at least 10 responses. Thegreatdr ( talk) 16:18, 9 May 2008 (UTC)
As part of the WikiProject Good Articles, we're doing sweeps to go over all of the current GAs and see if they still meet the GA criteria. I'm specifically going over all of the "Meteorology and atmospheric sciences" articles. I believe the article currently meets the criteria and should remain listed as a Good article. I have made several minor corrections throughout the article. Altogether the article is well-written and is still in great shape after its passing in 2007. Continue to improve the article making sure all new information is properly sourced and neutral. It would also be beneficial to go through the article and update all of the access dates of the inline citations and fix any dead links. If you have any questions, let me know on my talk page and I'll get back to you as soon as I can. I have updated the article history to reflect this review. Happy editing! -- Nehrams2020 ( talk) 04:59, 14 June 2008 (UTC)
Under the heading "Remote Sensing", there are a number of images under the sub-heading "Satellite Images of Selected Tropical Storms and Associated T-Number". Below the images, there is the name of the storm and a T-Number such as "Hurricane Emily at T6.0". There is no explanation what these T-Numbers are. The same issue occurs on the page Maximum_sustained_wind (with the same images - I left a comment on that page as well). SmilingBoy ( talk) 11:14, 1 September 2008 (UTC)
Lighter oxygen isotopes (18O) are left behind in coral during periods of very heavy rainfall. Wait, isn't O18 the HEAVIEST stable oxygen isotope? 32ieww ( talk) 23:21, 18 March 2017 (UTC)
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