MW 3 PART 2 DELAYED DUE TO CHANGING SITUATION. WILL BE PUBLISHED ON WEDNESDAY NIGHT.
Vagaries© of the weather.blog written by rajesh kapadia.concentrating on meteorology of the Indian sub continent and extreme world weather since 55 years For Any Information taken from here, due credit must be given to Vagaries.
Monday, May 07, 2018
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Weekend outlook; 20th/21st/22nd April Mumbai : Dry heat gone...warm stuffy discomfort coming ! After seeing blistering heat last week at 38/...
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Wettest Monsoon Day in 2013 for maharashtra...See pradeep's Page BB-4 lingers on, and on Tuesday, was located as a weak low over N...
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Pune recorded 87 mm ending 8.30am today. With this achieved 1000 mm mark! Seasonal Rainfall stands on 1018 mms now. Last night Widespread...
2 comments:
Lets hope changes are positive :-)
Credit Australian government bureau of meteorology
Issued 8 May 2018
The latest ENSO Wrap-Up and Climate Model Summary are now available on the Bureau's website.
Tropical Pacific remains El Niño–Southern Oscillation neutral
The El Niño–Southern Oscillation (ENSO) remains neutral, with neither El Niño nor La Niña in the tropical Pacific Ocean. International models suggest it will remain neutral through at least the southern hemisphere winter.
Atmospheric and oceanic indicators of ENSO are generally at near average levels. Sea surface temperatures (SSTs) are close to the long-term average across the tropical Pacific Ocean, and waters beneath the surface are slightly warmer than average. In the atmosphere, the Southern Oscillation Index (SOI) and trade winds are both within the neutral range.
International models suggest the tropical Pacific Ocean will warm slowly over the coming months, but remain ENSO-neutral for the southern hemisphere winter. Only one of eight climate models suggest sea surface temperatures may approach El Niño thresholds by September; the rest maintain ENSO-neutral.
The Indian Ocean Dipole (IOD) is currently neutral. Half the surveyed climate models suggest the IOD will remain neutral for winter, while the other half predict a negative IOD. However, the present above average SSTs off northwest Australia are a result of reduced cloud cover increasing solar warming. If this pattern persists, a typical negative IOD response, such as more cloud off northwest Australia, is less likely. During negative IOD events, winter–spring rainfall is typically above average over southern Australia.
More information
Media enquiries: (03) 9669 4057 media@bom.gov.au
Next update expected on 22 May 2018
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