Sentences with phrase «warm sea conditions»

The popularity of Mexico fishing vacations in Riviera Nayarit is largely due to the exceptional climate and warm sea conditions found in this Pacific coast region, which are always very favourable.

The summer season is the busiest, with warm sea conditions that invite a wide variety of water activities.

Not exact matches

Two major factors are creating hurricane - friendly conditions in the Atlantic region, which includes the Caribbean Sea and Gulf of Mexico: warm water and a lack of wind shear.

You need warm sea - surface temperatures, an environment of low wind shear, high humidity — and those are just a few of the conditions.

Sea surface temperatures in the Pacific Ocean are warmer than normal — El Niño conditions — which suppress rainfall in the eastern Amazon.

Conclusion: Global warming was primarily responsible, due equally to the thinning sea ice and warm atmospheric conditions.

The study examined 27 years worth of satellite data for sea surface temperatures, previous coral bleaching events, and studied how corals responded to different seawater warming conditions.

A study examined three different factors: warmer - than - usual surface atmosphere conditions (related to global warming); sea - ice thinning prior to the melting season (also related to global warming); and an August storm that passed over the Arctic, stirring up the ocean, fracturing the sea ice and sending it southward to warmer climes.

GOING, GOING... Warmer conditions in the Arctic are melting sea ice (as seen here near Barrow, Alaska).

Professor Grant Bigg, from the University's Department of Geography, said: «Many people may associate warmer seas with the pleasant weather conditions they're used to experiencing while on holiday, but the fact of the matter is that an increase in sea temperatures is having a huge impact on the world's weather.

Bacteria, however, have remained Earth's most successful form of life — found miles deep below as well as within and on surface rock, within and beneath the oceans and polar ice, floating in the air, and within as well as on Homo sapiens sapiens; and some Arctic thermophiles apparently even have life - cycle hibernation periods of up to a 100 million years while waiting for warmer conditions underneath increasing layers of sea sediments (Lewis Dartnell, New Scientist, September 20, 2010; and Hubert et al, 2010).

Long - term (decadal and multi-decadal) variation in total annual streamflow is largely influenced by quasi-cyclic changes in sea - surface temperatures and resulting climate conditions; the influence of climate warming on these patterns is uncertain.

The accessibility of a large numbers of tidewater glaciers, subject to warming conditions, provides a unique opportunity to observe processes and enable more accurate predictions of sea level response to ocean warming around Antarctica.

Climate conditions favor warm water growth — as measured by sea surface temperature (SST)-- later in the year, suggesting that normal climate conditions effectively nipped the nascent El Niño in the bud.

This new group of scientists find some weather disturbances were not from the El Nino, La Nina cycle, but apparently regulated by conditions in the Arctic — things like low sea ice, low or shorter season snow cover, and even «sudden stratospheric warming».

This chemical weathering process is too slow to damp out shorter - term fluctuations, and there are some complexities — glaciation can enhance the mechanical erosion that provides surface area for chemical weathering (some of which may be realized after a time delay — ie when the subsequent warming occurs — dramatically snow in a Snowball Earth scenario, where the frigid conditions essentially shut down all chemical weathering, allowing CO2 to build up to the point where it thaws the equatorial region, at which point runaway albedo feedback drives the Earth into a carbonic acid sauna, which ends via rapid carbonate rock formation), while lower sea level may increase the oxidation of organic C in sediments but also provide more land surface for erosion... etc..

Mengel said some simulations produced the warm ocean conditions needed to remove the ice cork within the next 200 years, but It would take around 2,000 years to raise global sea levels by one meter (3.3 feet).

Guest rooms have a warm homely decor with light wood furnishings and modern amenities for your comfort; features include a private furnished balcony or terrace with lateral sea view, air - conditioning (from 1st June until 30th Sept), private bathroom with hair dryer, twin queen beds, satellite TV, telephone, mini fridge and safe box.

Guest rooms of spacious design have a smart attractive decor of pale interiors, drapes of warm colour and patterned bed covers to complement, light wood furnishings on cool tiled flooring and modern amenities for your comfort; features include a private furnished balcony with sea view, air - conditioning, en suite bathroom with separate bathtub and shower, separate wc, make - up mirror and hair dryer, lounge area with sofa bed, flat screen satellite TV, telephone, piped music, internet connection charge), desk and seating, table and seating, mini fridge and a mini bar and safe box on request (charge).

Guest rooms in the Iberostar Malaga Playa Hotel have a warm Mediterranean decor, soft pastel interiors with complementing drapes and fabrics, comfortable wood - style furnishings on carpeted flooring with modern amenities for your well - being; features include a private furnished balcony or terrace, some with sea views, centrally - controlled air - conditioning, satellite TV, music channel, telephone and a mini fridge.

Excellent conditions, trade winds almost every day of the year, a relaxing atmosphere and warm waters from the Caribbean Sea make Bonaire a perfect destination for kite boarders of all levels.

While warm waters do make conditions good for swimming, visitors are advised to be on their guard against strong currents that can draw even experienced swimmers out to sea.

We have selected inland fresh water lakes for their convenient locations, they make it easier to set up and equipment and enter the water, they are generally warmer than the sea and can be dived in all weather conditions.

Guest rooms are designed for your comfort and relaxation, with a warm décor and good standard of amenities; features include air - conditioning, a balcony (majority with sea view, or side sea view), private bathroom with hair dryer, cable TV, telephone, mini fridge, and child / baby cots available on request.

The abundant waters off the coast of Cabo San Lucas — located at the southern tip of the Baja Peninsula, where the calm and warm waters of the Sea of Cortez mixes with the unfathomable cool currents of the Pacific Ocean — offer the ideal conditions for plenty of sport - fish species, including (among others) Rooster Fish, Mahi Mahi (known locally as Dorado), varieties of Tuna, Sharks, Jacks, Groupers, and Billfish such as Sailfish, Swordfish, Black Marlin, Blue Marlin and Striped Marlin.

Guest suites have a trendy design and contemporary styling with a mix of pale and warm toned interiors, drapes and fabrics of vibrant colour, attractive wall - hung art, smart furnishings cleverly spaced on cool tiled flooring and modern amenities to take care of your comfort; features include a private furnished balcony for most suites with sea or marina view, air - conditioning, a private bathroom with hair dryer and amenities, living room with TV (international channels) and DVD player on request, DVD library at reception, sofa bed / armchair, a bedroom (s) with twin beds, writing desk and chair, telephone, night curtain, a kitchenette with 2 - ring hob, microwave, fridge, coffee machine, kettle, toaster, plates & cutlery and table with 4 chairs, iron and board, and baby amenities.

As the authors point out, even if the whole story comes down to precipitation changes which favor ablation, the persistence of these conditions throughout the 20th century still might be an indirect effect of global warming, via the remote effect of sea surface temperature on atmospheric circulation.

A subset of Earth System Models (ESMs) project that El Niño - like conditions will progressively increase in coming decades as sea - surface temperatures in the tropical Pacific warm, implying increased drought and forest dieback in the Amazon.

Soundbite version: «Global warming is expected to increase sea surface temperatures, create a thicker and warmer ocean surface layer, and increase the moisture in the atmosphere over the oceans — all conditions that should lead to a general increase in hurricane intensity and maybe frequency.»

Now to contribute a single event to Global Warming, one has to look at the weather conditions, and if patterns are sighted which are tied to alteration of sea ice decline (our new atmosphere set up), we can connect the dots here too.

«The climate patterns responsible for the expected above - normal 2007 hurricane season continue to be the ongoing multi-decadal signal (the set of oceanic and atmospheric conditions that have spawned increased Atlantic hurricane activity since 1995), warmer - than - normal sea surface temperatures in key areas of the Atlantic Ocean and Caribbean Sea, and the El Nino / La Nina cycle&raqsea surface temperatures in key areas of the Atlantic Ocean and Caribbean Sea, and the El Nino / La Nina cycle&raqSea, and the El Nino / La Nina cycle»

«in Western Hudson Bay, the decline in population size, condition, and survival of young as a consequence of earlier breakup of the sea ice brought about by climate warming have all been well documented (Stirling et al., 1999; Gagnon and Gough, 2005; Regehr et al., 2005; I. Stirling and N.J. Lunn, unpub.»

But this is in a period that the Bureau has predicted is likely, based on statistical analysis of historical data and current sea surface conditions, to be warmer than the historical average (see here.

It is also possible for cold climates to increase chemical weathering in some ways, by lowering sea level to expose more land to erosion (though I'd guess this can also increase oxydation of C in sediments) and by supplying more sediments via glacial erosion for chemical weathering (of course, those sediments must make it to warmer conditions to make the process effective — downhill and downstream, or perhaps via pulsed ice ages -LRB-?)-RRB-.

El Nino is characterised by warmer than normal sea surface along the equator in the eastern Pacific, whereas La Nina is colder than normal conditions over the same region.

With respect to Antarctic sea ice Zhang 2006 «Increasing Antarctic Sea Ice under Warming Atmospheric and Oceanic Conditions.&raqsea ice Zhang 2006 «Increasing Antarctic Sea Ice under Warming Atmospheric and Oceanic Conditions.&raqSea Ice under Warming Atmospheric and Oceanic Conditions.»

I've sent a query to some hurricane researchers to get a bit more on what, besides warm sea temperatures, makes conditions this ripe for powerful tropical storms.

Apparently in warmer, superanoxic conditions some sea bacteria turn CH4 into H2S (hydrogen sulfide) which kills life, and is thought to have nearly done in what meager life remained during the end - Permian 251 mya after serious 6 - 8C warming over 10000s of years did a nasty job on life.

«Near - bottom water warming in the Laptev Sea in response to atmospheric and sea - ice conditions in 2007&raqSea in response to atmospheric and sea - ice conditions in 2007&raqsea - ice conditions in 2007»

But efforts to tease out the impact of human - driven global warming in the region are complicated by the big influence around the Bering Sea of natural variations in ocean conditions, including the Pacific Decadal Oscillation.

There are a variety of debates under way over the merits or perils of focusing on particular climate (and sea level) findings, or a particular season's conditions, in discussing human - driven global warming.

As I've written before, while 20 years of intensifying inquiry has greatly reinforced confidence that humans are influencing climate in ways that could profoundly disrupt human and natural affairs, it has not substantially clarified climate outcomes that matter most: how fast and far temperatures and seas will rise in the next 100 years, how hurricanes will respond to warming, how regional conditions will change.

That approach, from Katrina forward, was bound to fail, given the variability of conditions year to year and persistent (and non-manufactured) uncertainty surrounding some of the most consequential impacts (for instance, the pace and extent of warming and sea - level rise in this century).

They then looked at the challenges that warmer oceans delivered for crustaceans, molluscs, sponges, deep sea invertebrates, the warm and cold water corals that provide habitat for one - fourth of the ocean's variety, the pelagic or surface - swimming fish, and the demersal or deep - sea denizens that live longer, reproduce more slowly and are thus less likely to evolve and adapt to changing conditions.

Shorefast ice conditions along the northeastern Chukchi Sea coast (Barrow to Wainwright) reflect the combination of late freeze - up after the 2012 record minimum summer ice extent and persistent westerly flow advecting warm air throughout fall and early winter.

The traditional approach is to fix the sea surface temperature (SST) and free - tropospheric conditions, which are then perturbed to mimic global warming (e.g., Rieck et al. 2012; Blossey et al. 2013).

Warmer winter conditions, for instance, have the potential to benefit alewife, round gobies, ruffe, sea lamprey, rainbow smelt, and other non-native species.

Warm melts Arctic Sea Ice and turns the Air Conditioning on.

For the sea of humanity that is increasingly feeing the changing conditions resulting from a warmer climate brought on by anthropogenic interference, it is clear what must be done — reduce emissions dramatically in the developed countries.

Sea ice, and the cold conditions it sustains, serves to stabilize methane deposits on and near the shoreline, [40] preventing the clathrate breaking down and outgassing methane into the atmosphere, causing further warming.