You've
got warm tropical waters and the Great Barrier Reef in the north, Australia's best collection of beaches along the central east coast and towering cliffs in the south.
Not exact matches
A must visit location with
warm waters, a
tropical climate, and a huge selection of mellow beach breaks and intense reef breaks have Costa Rica is widely regarded as the perfect Winter
get away for European surfers and travellers.
When you add in
warm tropical water, and a charming town filled with yoga studios, boutiques and restaurants, it's a great place to
get away from it all.
So if you dream of overhead surf,
warm water with greeny palm trees as a view and offshore breezes everyday on
tropical island paradise with LOW BUDGET journey, you may stay and surf with us
get your choice at BUDGET MENTAWAI SURFCAMP.
You will
get opportunity to explore the mature
tropical gardens, towering trees and palms and also the soft iridescent sand beach with clear
warm water.
Wally the Maori Wrasse and his mob
get around, not content to hang out in the
warm waters of
Tropical North Queensland, Wally's hump headed cousins have been spotted in the Whitsundays too.
The year - round
warm tropical waters of the Bahamas make ideal conditions for coral reef growth, and on our coral reef dives you will
get a chance to explore some of the dozens of awesome reef sites located around Nassau!
Other factors would include: — albedo shifts (both from ice >
water, and from increased biological activity, and from edge melt revealing more land, and from more old dust coming to the surface...); — direct effect of CO2 on ice (the former weakens the latter); — increasing, and increasingly
warm, rain fall on ice; — «stuck» weather systems bringing more and more
warm tropical air ever further toward the poles; — melting of sea ice shelf increasing mobility of glaciers; — sea
water getting under parts of the ice sheets where the base is below sea level; — melt
water lubricating the ice sheet base; — changes in ocean currents -LRB-?)
Yes, to
get a really good
tropical storm, you need
tropical warm waters and an arctic airflow above it, giving a huge temperature gradient in the atmosphere (low level
warm air and freezing air above).
With a rise in the overall temperature of the ocean, ocean - borne storms such as
tropical storms and hurricanes, which
get their fierce and destructive energy from the
warm waters they pass over, could increase in force.
The
warm water and calm winds of this periodic Pacific
tropical condition are «a big way to
get subsurface heat back to the surface.»
The
warmer the
water, the more energy
gets sucked in the air and the faster a
tropical cyclone develops into a hurricane and the more powerful this hurricane can grow — other complex meteorological factors left aside.
It's well - known that
tropical cyclones need surface
water temperatures of at least 26.5 °C (80 °F) to maintain themselves, and that the
warmer the
water, and the deeper the
warm water is, the stronger the storm can
get.
I suspect that 3 - year La Niña lasted so long because there was so much
warm water in the western
tropical Pacific (that was left over from the 1997/98 El Niño) that the
tropical Pacific simply
got stuck in La Niña mode until the
warm water was distributed and dissipated.
You wrote, «Since the variations in the Nino 3.4 index are indicative of the functioning of one of the Earth's major thermoregulating mechanisms, namely the giant El Nino / La Nina pump that magically materializes to move
warm tropical Pacific
water to the poles whenever the planet
gets too hot and sweaty... then under what possible construction could the Nino 3.4 Index variations be called «noise»?»
«Obviously the hotter
water deep under the ice at the poles did not
get any heat from the sun to be
warmer and does not all have
tropical water currents heating it, so where does the deep
water get its heat from to stop from freezing.»
De Witt, are you saying «THS???» because you don't know it stands for
tropical hot spot [which I can't believe] or because you don't
get the connection between backradiation and a THS, which I understood to be the case because the Troposphere would
warm faster than the surface since it is being heated by a
warmer surface, to wit, the surface of the planet which is
getting warmed by the aforesaid backradiation; and in addition to but not withstanding that the troposphere whould also rise which would be another aspect of the THS, with the final characteristic being that said THS would occur in the tropics where the
warming effect of extra
water would be most pronounced, also as a consequence of backradiation?
The fact is, is that NOAA, in the federal government, has shown that there is conclusive evidence that the
tropical waters are
getting warmer as a result of global
warming and while that doesn't lead to more hurricanes, what it leads to is more intense, and and hurricanes, hurricanes that are more intense.
But once the
water vapor in the parcel reaches saturation some of this vapor condenses and releases its latent heat, compensating for some of the cooling (you
get about 45K of
warming from latent heat release when a typical parcel rises from the
tropical surface to the upper troposphere).