Sentences with phrase «by warm tropical waters»

You'll be surrounded by warm tropical waters and spectacular ocean views.

Not exact matches

Japan, the east coast of the US, northern Brazil and south eastern Africa are also strongly influenced by coastal currents that transport warm tropical waters.

The next step was see how those factors were influenced by ENSO; while El Niños and La Niñas are defined by how much warmer or colder than normal tropical Pacific ocean waters are, they trigger a cascade of reactions in the atmosphere that can alter weather patterns around the globe.

Last year's devastating category - 5 hurricane — Matthew — may be one of many past examples of a tropical storm fueled by massive rings of warm water that exist in the upper reaches of the Caribbean Sea.

El Niño, a periodic warming in the waters of the eastern tropical Pacific Ocean, will probably emerge in the coming months, according to a forecast issued yesterday by the Climate Prediction Center (CPC) of the National Oceanic and Atmospheric Administration (NOAA).

Though El Niño is defined by the warmer - than - normal ocean waters in the eastern tropical Pacific, it is a phenomenon with a global reach.

La Niña is the opposite end of the natural climate seesaw from El Niño; it is characterized by cooler - than - normal ocean waters in the tropical Pacific, while El Niño features warmer - than - normal.

El Niño, marked by a warm patch of water in the eastern tropical Pacific, influences a number of weather patterns around the world.

The warm waters across the central and eastern tropical Pacific are boosting global temperatures, which is on top of the long - term warming driven by human greenhouse gas emissions.

In the tropical Pacific, the distance from Indonesia to South America and the way tropical winds push warm water west combine to allow special waves to travel along the equator and are amplified by the atmospheric wind response to produce large fluctuations in temperatures (up to 3 degrees Celsius) in the Eastern Pacific that last for months.

In any year, temperatures around the world can be nudged up or down by short - term factors like volcanic eruptions or El Ninos, when warm water spreads over much of the tropical Pacific Ocean.

Salty Bird Swimwear — Inspired by the constant surf, warm waters and tropical beaches of Costa Rica, Salty Bird Swimwear is a functional, feminine, and foxy surf bikini.

South Water Caye Imagine an island less than a half mile long, covered with white coral sand, tropical flowers, and coconut trees, surrounded by warm, crystal clear water enveloped in coral reefs that wrap more than half way around the isWater Caye Imagine an island less than a half mile long, covered with white coral sand, tropical flowers, and coconut trees, surrounded by warm, crystal clear water enveloped in coral reefs that wrap more than half way around the iswater enveloped in coral reefs that wrap more than half way around the island.

If salt is in your veins, Mackay is within 31 beautiful beaches, ranging from patrolled swimming spots just minutes from the city centre, spectacular coastal national parks, to miles of untouched coastline, all lapped by the warm, tropical waters of the Coral Sea.

When people think of Pacific diving, the first things that pop into their minds are exquisitely beautiful tropical islands, clear, warm water and lush coral reefs — populated by colorful fish and visited by awesome pelagics.

The narrow beach is made up of golden sand peppered with large rocks, giving it a natural untouched feel, and is lined by shade - providing tropical trees on one side and clean warm waters on the other side.

As a selected temporary «Calivigny Island Proprietor» you own and offer to your family, your guests and friends an exquisite holiday home surrounded by white sandy beaches, lush tropical gardens and warm crystal clear waters.

- Beautiful, tropical island to call home - Best Freediving facilities in the world (built by Freedivers for Freedivers)- One of the busiest Freediving schools worldwide - Dedicated team of Instructors and Athletes — eager training buddies always available - Unlimited depth — yoga studio on site -25 m swimming pool - Warm water (27 - 31 degrees throughout the...

Mexico's Riviera Maya is a stunning expanse of perfect, sparkling white sand, bathed by the warm, turquoise - clear waters of the Caribbean Sea, dotted with swaying coconut palms, and soaked by the rays of a tropical sun...

Blessed with a warm tropical climate and featuring many picturesque beaches fringed with coconut trees and lapped by turquoise clear waters, you have a chance to spend a great time in a postcard - like environment at well below rack - rates.

These 420 square feet suites are perfect for travelers in search of an exclusive tropical vacation by the warm blue waters of the Caribbean Sea.

Situated on the waters edge with endless views across the sparkling coral sea, grand mercure apartments magnetic island is the place where you and your tropical dreams meet — a private retreat nestled amongst pristine, natural island beauty - caressed by gentle sea breezes and bathed in a warm, tropical climate.

The country narrows through a chain of increasingly tropical provinces washed by the warm waters of the East Sea.

With its warm clear waters crammed with colourful, tropical fish - life and corals, set around stunningly beautiful tropical islands, the Andaman Sea boasts some high quality scuba adventures and certainly offers the best diving in Thailand by far.

The beaches are white with crystal clear water that is flat and calm and protected by offshore reefs that provide fun for the surfers and a variety of waterborne activities for everyone else that can be conducted in the lagoons of warm tropical waters.

The tropical, turquoise water is warm and scenic surf spots dot the bays, many surrounded by massive headlands and cliffs.

Benoa Beach is one of the recommende beaches in Bali where warm turquoise clear waters meet white sands that are sheltered by palms and other tropical trees.

Without going into technical details about the dynamics and thermodynamics involved in tropical storms and hurricanes (an excellent discussion of this can be found here), the basic connection between the two is actually fairly simple: warm water, and the instability in the lower atmosphere that is created by it, is the energy source of hurricanes.

In the progression of tropical disturbance > tropical storm > hurricane the available energy is limiting the growth of the system; unless the vertical structure of the hurricane engine is blown apart by winds, the thing will grow when it hits a warm deep water zone.

Conceptually, it's hard to see how the Gulf Stream western boundary current could be weakened by conditions around Greenland; this is a fluid dynamics system, not a mechanical «belt»; a backup due to less deep water formation should have little effect on the physics of the gyre and the formation of the western boundary current, and it also seems the tropical warming and the resulting equator - to - pole heat transport are the drivers — but perhaps modulation by jet stream meandering is playing some role in the cooling?

A recent, widely publicized research study has suggested that the ocean's «thermohaline» circulation that keeps the Earth's north polar region warmed by the flow of tropical water northward could suddenly shut down.

All the sea surface water, warmed by the tropical sun, is blown to the west of the Pacific and, to compensate part of the imbalance, cooler deep ocean waters well up on the western shores of Latin America (and spread all the way up to the Solomon Islands).

Warm tropical water forced by tides and Coriolis effect into a bottleneck created by a land mass funnel causes a small sensible energy fluctuation that drives folks absolutely nuts trying to figure it out.

The latter is marked by a pool of warm water in the tropical Pacific that sets off a domino effect in the atmosphere that shifts the jet stream around over the U.S.

4) By interpreting the analyss of Bob Tisdale, the global sea surface temperatures used by Endersbee in his calculations have been controlled by warming of the sea surface waters outside the tropical sea surface i.e. mainly by the warming of the sea surface waters of higher latitudes where the sea surface CO2 sinks arBy interpreting the analyss of Bob Tisdale, the global sea surface temperatures used by Endersbee in his calculations have been controlled by warming of the sea surface waters outside the tropical sea surface i.e. mainly by the warming of the sea surface waters of higher latitudes where the sea surface CO2 sinks arby Endersbee in his calculations have been controlled by warming of the sea surface waters outside the tropical sea surface i.e. mainly by the warming of the sea surface waters of higher latitudes where the sea surface CO2 sinks arby warming of the sea surface waters outside the tropical sea surface i.e. mainly by the warming of the sea surface waters of higher latitudes where the sea surface CO2 sinks arby the warming of the sea surface waters of higher latitudes where the sea surface CO2 sinks are.

The Atlantic Meridional Overturning Circulation (AMOC)- the transport of warm tropical surface water northward - is indeed propelled by dense water sinking in the North Atlantic and travelling equatorward in the deeper layers, but it also has a wind - driven component to it.

During high solar output of the Medieval Warm Period, tropical waters in both the Atlantic13 and Pacific14 increased by as much as 1 °C warmer than today.

Which forms the basis for the IPCC claim of high climate sensitivity (mean value of 3.2 C), resulting in significant global warming (up to 6.4 C warming by 2100), «extreme high sea levels», increased «heat waves», increased «heavy rains» and floods, increased «droughts», increased «intense tropical cyclones» — which, in turn, lead to crop failures, disappearance of glaciers now supplying drinking water to millions, increased vector borne diseases, etc. (for short, potentially catastrophic AGW — or «CAGW»).

As the air rises, it expands and cools, and water vapour condenses, releasing even more heat,» much like how a hurricane frees energy by drawing warm humid air from its base (usually tropical sea water) and then releasing cold, wet air 7 miles (12 kilometers) up in the troposphere.

The rise in tropical Pacific OHC was not caused by a transfer of warm waters from another basin, Stephen.

Hurricanes (Fig. 7) and other tropical cyclones can be thought of as heat engines that take energy in by evaporating warm ocean water, and eject it at a colder temperature near the tropopause after air rises and water condenses in the eyewall [14].

The layer of warm surface water that was blown west is then replaced by cooler water from the subsurface, cooling the entire tropical Pacific.

Part of the upward shift is caused by the warm water returned to the western tropical Pacific by the Rossby wave.

El Nino is characterized by warm water across the tropical Pacific.

The effects of tropical cyclones early in the year were followed by regular northwest cloud - band activity between May and mid-July, when waters northwest of the continent were unusually warm as part of a negative phase of the Indian Ocean Dipole.

Scientists say the tropical storm was likely intensified by climate change: rising sea levels means larger storm surges, warmer ocean waters cause more precipitation, and unseasonal weather means hurricane season may be lasting longer.

In any year, temperatures around the world can be nudged up or down by short - term factors like volcanic eruptions or El Ninos, when warm water spreads over much of the tropical Pacific Ocean.

In order of seniority, the seven feedbacks that seem outstanding are: Water vapour — rising by ~ 7 % per 1.0 C of warming; Albedo loss — due mostly to cryosphere decline; Microbial peat - bog decay — due to rising CO2 affecting ecological dynamics; Desiccation of tropical and temperate soils — due to SAT rise and droughts; Permafrost melt — due to SAT rise plus loss of snow cover, etc; Forest combustion — due to SAT rise, droughts, pest responses, etc; Methyl clathrates [aka methane hydrates] now threatened by rising sea - temperatures, increased water column mixing, Water vapour — rising by ~ 7 % per 1.0 C of warming; Albedo loss — due mostly to cryosphere decline; Microbial peat - bog decay — due to rising CO2 affecting ecological dynamics; Desiccation of tropical and temperate soils — due to SAT rise and droughts; Permafrost melt — due to SAT rise plus loss of snow cover, etc; Forest combustion — due to SAT rise, droughts, pest responses, etc; Methyl clathrates [aka methane hydrates] now threatened by rising sea - temperatures, increased water column mixing, water column mixing, etc..

In the tropical Pacific, the distance from Indonesia to South America and the way tropical winds push warm water west combine to allow special waves to travel along the equator and are amplified by the atmospheric wind response to produce large fluctuations in temperatures (up to 3 degrees Celsius) in the Eastern Pacific that last for months.

It means that the global sea surface temperatures used by Endersbee in his calculations have been controlled by warming of the sea surface waters outside the tropical sea surface i.e. mainly the warming of the sea surface waters of higher latitudes where the sea surface CO2 sinks are.