Because of their longer exposure to the
large warm pool, their winds had 50 to 80 percent more destructive power, and they brought 30 to 50 percent more heavy rain.
For the older kids there were about a half dozen thrill slides, plus there's an adults
only warming pool.
Mehta, V. M., and H. Wang, 2010: Interannual variability of the West Pacific and West Atlantic
warm pools in remote sensing based and ECCO - assimilated oceanographic data sets.
Wang, C., H. Liu, S. - K. Lee, and R. Atlas, 2011: Impact of the
Atlantic warm pool on United States landfalling hurricanes.
Consistent with previous studies, the team also found that Rossby gyres associated with a previous MJO event help to initiate the next cycle by moistening the atmosphere in the western part of the Eastern Hemisphere
ocean warm pool before the new MJO heads east.
Thus, during an El - Nino, much of the heat content of the Indo - Pacific
warm pool moves from being too deep for surface measurements to detect, to being spread out on the surface of the ocean, where surface measurements can detect it.
The presence of the 30 year
PDO warm pool will tend to favour La Nina over El Nino events which regulates Earth's climate.
Every two to seven years, an
unusually warm pool of water — sometimes two to three degrees Celsius higher than normal develops across the eastern tropical Pacific Ocean to create a natural short - term climate change event.
Other possible activities: Soaking, bathing and swimming in
natural warm pools, by the ocean.
There was a huge play structure that dumps a giant bucket of water every few minutes, two enclosed play spaces for infants through preschoolers, a pool with lily pads and basketball nets, a large wave pool (this was a huge hit for all of us), a
family warming pool, a lazy river, and 4 short slides for age 1 - 6 years.
The larger
warm pool gave the simulated hurricanes more time to grow before they encountered colder water or land.
This is not surprising as the Indian Ocean is linked to El Niño's
warm pool by a current called the Indonesian through - flow.
Without the constant force of the wind to hold the warm waters back, the West Pacific
warm pool begins to migrate easterly as the sea - surface level begins to equalize, an event termed an «El Niño / Southern Oscillation» (ENSO).
During an El - Nino, the Indo - Pacific
warm pool becomes less deep, and spreads out across the Pacific.
Lavish in luxurious hammams or sink into open - air cold and
warm pools for peaceful relaxation.
You will find dozens of cascading waterfalls and
warm pools along the riverbed, of varying temperatures, water flows and degree of privacy.
After so much repetition and reiteration though, even a soaring high camp wit can so easily plummet into the shallow
luke warm pool of the just plain twee.
There is a
largish warm pool across the entire Gulf of Mexico right now — that might have something to do with it:
If we apply that same reasoning to Ike (take a look at that big eastern
GOM warm pool), then this one is probably going to be far more devastating.
A further point where I need clarification is that, in Part I, you seemed to be suggesting that the West Pacific
warm pool develops due to the trade winds blowing surface water in that direction.
«Our results from this study imply that if future anthropogenic warming effects in the Indo - Pacific
warm pool dominate natural variability, mid-ocean islands such as the Mascarenhas Archipelago, coasts of Indonesia, Sumatra, and the north Indian Ocean may experience significantly more sea level rise than the global average,» Han said.
Then you can look at the Oppo 2009 indo - pacific
warm pool reconstruct which has an excellent fit with the instrumental oscillations and that recovery pattern extends to 1700 in that reconstruction.
As the central part of the Pacific warms up during El Niño, the atmospheric convection that normally occurs over the western
warm pool migrates to the central Pacific.
In effect, the researchers say, the missing heat from global warming is being stored in a deeper
warm pool in the western Pacific.
«While La Niña [conditions in 2011] had a large role to play in the failure of the rains in East Africa, there is evidence that warming in the western Pacific — Indian
Ocean warm pool has contributed to an increased frequency of droughts in this region,» the researchers note.
The neg
PDO warm pool was responsible for the last stage of the back to back La Nina of 2010/11.