Sentences with phrase «on warmer surface waters»

It is interesting to note that the AMO explanation still relied on warmer surface waters as the root cause of hurricane intensification.

Not exact matches

The planets orbit an «ultracool dwarf,» a star much smaller and cooler than the sun, but still possibly warm enough to allow for liquid water on the surfaces of at least two of the planets.

1) Sift the flour into a mixing bowl 2) Add the salt to the flour, mixing together 3) Add the olive oil, mixing as you add to ensure the flour envelopes the oil 4) Add warm water bit by bit until dough reaches the right consistency 5) One the dough ready, roll it into a ball, and knead well on a cool, flat surface 6) Flatten the dough with a wooden rolling pin 7) Cut into 10 cm pieces and roll them long enough and evenly 8) Place the pin - shaped dough on a well - greased baking tray 9) Bake in oven at 175 deg cel (medium heat for gas ovens) for 20 -30 minutes or until the sticks are ready (test by breaking off a small piece to check that the inside is well cooked) 10) Allow to cool for 5 minutes before serving

Make Pretzel Dough: Stir together warm water and yeast in a large bowl and let stand until a creamy beige foam develops on the surface, about 10 minutes.

I took the dough out of the bowl and flattened it on a floured surface, kneading it lightly to get the air out, and repeated the rising process; placed the dough in the bowl, covered, filled sink with warm water, and placed the bowl in sink.

Dip a rice paper wrapper into warm water and immediately pull it out of the water, letting the excess moisture drip off before placing on a clean surface.

1) Mix flour, butter and icing sugar in a bowl using two knives to cut the butter until the mixture resembles fine breadcrumbs 2) Add in the egg yolks and vanilla extracts and mix well, then add iced water until the dough starts to come together 3) Shape the dough into a ball on a cool, flat, floured surface 4) Flatten dough into a disc and then wrap in plastic wrap, and chill in the refrigerator for at least 30 minutes 5) Meanwhile, peel, core and slice the apples into as thin slices as possible 6) Mix sugar and ground cinnamon powder with sliced apples and let it rest for a while 7) Pre-heat oven to 180 deg cel 8) Once dough has chilled, roll pastry dough on a sheet of parchment paper until it has expanded to the size of the tart mold (I used a rough mold the size of a large pizza) 9) Leaving at least an inch of dough free, arrange apple slices by overlapping them slightly in the shape of a circle, starting from the outermost part of the circle, until you reach the inside 10) Fold the edges of dough over the filling and then sprinkle the dough with a bit of sugar 11) Bake for about 40 - 45 minutes, or until the crust is golden brown and the apples are soft 12) Serve warm, with a side of whipped cream or ice cream (optional)

To make each roll, simply wet a sheet of rice paper with warm water and lay it on a flat working surface, like a cutting board.

This is accomplished with a powerful blast of warm air that quickly breaks up the layer of surface water on a userâ $ ™ s hands for quick removal and evaporation.

In Martian summer, the combination of warm temperatures and a thin atmosphere make any liquid water on the surface boil, which can let dust hover across the ground

MAVEN arrived at Mars in Sept. 2014 on a mission to investigate a planetary mystery: Billions of years ago, Mars was blanketed by layer of air massive enough to warm the planet and allow liquid water to flow on its surface.

SEAS researchers suggest that early Mars may have been warmed intermittently by a powerful greenhouse effect, possibly explaining water on the planet's surface billions of years ago.

In a paper published in Geophysical Research Letters, researchers found that interactions between methane, carbon dioxide and hydrogen in the early Martian atmosphere may have created warm periods when the planet could support liquid water on the surface.

Using the Large Binocular Telescope Interferometer, or LBTI, in Arizona, the HOSTS Survey determines the brightness and density of warm dust floating in nearby stars» habitable zones, where liquid water could exist on the surface of a planet.

The Michigan Tech chamber works differently due to cloud mixing between a hot and cold surface, the same process that forms clouds or fog over a lake on fall days when the water temperature is warmer than the air temperature.

The Michigan Tech chamber creates clouds through cloud mixing between a hot and cold surface — the same process that forms fog over Portage Lake on fall days when the water temperature is warmer than the air temperature.

Most climatologists expect that on average the atmospheres water vapor content will increase in response to surface warming caused by the long - lived greenhouse gases, further accelerating the overall warming trend.

Experiments carried out in the OU Mars Simulation Chamber — specialised equipment, which is able to simulate the atmospheric conditions on Mars — reveal that Mars» thin atmosphere (about 7 mbar — compared to 1,000 mbar on Earth) combined with periods of relatively warm surface temperatures causes water flowing on the surface to violently boil.

El Nino's mass of warm water puts a lid on the normal currents of cold, deep water that typically rise to the surface along the equator and off the coast of Chile and Peru, said Stephanie Uz, ocean scientist at Goddard Space Flight Center in Greenbelt, Maryland.

It's unclear whether this year's strong El Niño event, which is a naturally occurring phenomenon that typically occurs every two to seven years where the surface water of the eastern equatorial Pacific Ocean warms, has had any impact on the Arctic sea ice minimum extent.

One intriguing possibility: If fluid water does persist on Mars, life that might have thrived there millions of years ago, when the climate was warmer and wetter, could be hanging on in thin layers of salty water just beneath the surface.

«Near - surface waters around South Georgia [are] some of the fastest warming on Earth,» the new study says.

The study marks the first time that human influence on the climate has been demonstrated in the water cycle, and outside the bounds of typical physical responses such as warming deep ocean and sea surface temperatures or diminishing sea ice and snow cover extent.

Researchers identify such planets by first looking for those that are situated within the «habitable zone» around their parent stars, which is where temperatures are warm enough for water to pool on the surface.

A lot of evidence points towards Mars being warm and wet early in its history; features that look like rivers, lakes and outflows have been spotted both from orbit and by rovers on the surface, and a lot of the planet's minerals contain water.

With lots of warm surface water releasing heat into the atmosphere, in addition to ever - rising levels of greenhouse gases, 2015 is likely to surpass the warmest year on record, and 2016 will be similarly hot.

SEAS research suggests that early Mars may have been warmed intermittently by a powerful greenhouse effect, possibly explaining the presence of water on the planet's surface.

Under red dwarf stars, plant - type life on land may not be possible because photosynthesis might not generate sufficient energy from infrared light to produce the oxygen needed to block dangerous ultraviolet light from such stars at the very close orbital distances needed for a planet to be warmed enough to have liquid water on its surface.

With near - surface waters around South Georgia being some of the fastest warming on Earth climate change poses a significant threat to this biodiversity hotspot.

Looking at the chart, 53 planets (31 Warm Superterrans, 21 Warm Terrans, and one Warm Subterran) have the right size and temperature to potentially foster life, and exhibit features such as liquid surface on the water and a stable atmosphere.

In the East Pacific, the warm surface waters are a very shallow layer on top of the deep cold waters.

As a general matter, yes, but AIUI the increasing height (depth) of the ice face is the key factor for accelerating retreat of these glaciers since it creates more surface area for the warm water to work on.

At the extremely low surface temperatures on these objects, water ice takes a disordered, amorphous form instead of the regularly ordered crystals typical in warmer areas, such as snowflakes on Earth.

With its powerful suite of complementary science instruments, the mission soon revealed a towering plume of water ice and vapor, salts and organic materials that issues from relatively warm fractures on the wrinkled surface.

As an alternative, advise customers to melt a hole daily by setting a heated pan of warm water on the surface.

Winds at the time of the report on shore wind providing us with warm and clear water surface conditions.

The inversion itself is usually initiated by the cooling effect of the water on the surface layer of an otherwise warm air mass.

While the water on the surface is always warm you will need a 6 mm wetsuit for diving.

Bunaken National Park Located on the center of the coral triangle and created in 1991 Bunaken National Park covers a total surface area of 89,065 hectares, 97 % of which is clear, warm tropical water.

The increase in water vapour as the surface warms is key, but so might be changes in boundary layer stability, rossby wave generation via longitudinally varying responses at the surface, impacts of the stratopshere on the steering of the jet, and the situation is completely different again for tropical storms.

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-?)

On the other hand, decreasing stratospheric ozone (above 25 km), increasing stratospheric water vapor, and increasing atmospheric CO2 uniformly with height) will produce global surface and tropospheric warming along with stratospheric cooling.

If as a result of physical processes (such as El Nino) warmer water reaches the surface of the ocean, so less heat is conducted from the atmosphere into the ocean and the atmopsheric temperature will therefore increase — on a much shorter — comparatively instantaneous — timescale.

Climate models, on the other hand, have a successful track record — look at the melting Arctic, warming around Antarctica, the surface temperature, the water feedback effect, the reduction in mountain glaciers... etc..

Unlikely: this idea was based on the hypothesis that the Atlantic thermohaline circulation, which carries warm surface water to northern Europe, could be halted by the influx of fresh water from melting Arctic ice.

It stands to reason that the oceans haven't been that warm in a while but since the average temperature of the whole mass of water is so dependent on circulation (it's only the surface temperature that's constrained by its interactions with the atmosphere and space), I suppose a plausible history of that particular value would be very hard to reconstruct.

Suggested mechanisms range from upwelling of warm deep waters onto the continental shelf in response to variations in the westerly winds, to an influence of El Niño — Southern Oscillation on sea surface temperatures.

Reefs: Natural temperature - limiting processes may prevent ocean surface waters from warming past levels dangerous to corals, at least in some important regions, according to a study being published in Geophysical Research Letters on Saturday.

The increased area of warm water on the surface allows the tropical Pacific Ocean to discharge more heat than normal into the atmosphere through evaporation.

Before the ice gets too thick, the temperature contrast between the warmer water and the cold atmosphere makes conditions just right for the formation of surface crystals like this field of frost flowers on Dillon Reservoir, in the Rocky Mountains of Colorado.