It felt nice to have
the warm water flow toward me.
Warm water flowing through the Indonesian archipelago from the Pacific to the Indian Ocean influences the climate of the surrounding regions.
In this pattern,
warm waters flow northward from the tropics, then cool and become saltier and denser as they reach higher latitudes.
The region of the meltback is just inside the Bering Strait, where
warm water flows in from the Pacific, but in the analysis of Steele et al. this inflow of comparatively warm water was not particularly anomalous in 2007 relative to other years.
This ice shelf collapsed after 10600 years ago28, when
warmer waters flowed onto the continental shelf.
Looking at the Arctic ice event this year, it seems to me that a major part of that particular problem came with
warm waters flowing through the Bering Strait into the Arctic Sea.
The relatively
warm water flowing through the glacier also carries surface heat deep inside the ice sheet far faster than it would otherwise penetrate by simple conduction.
The job is done by
warm water flowing north from the tropics, variously called the Gulf Stream and, when nearing Ireland, the North Atlantic Current.
Sometimes the winds falter and
warm water flows back eastward suppressing cold upwelling.
Warm water flows between Australia and Indonesia influencing sea surface temperature in the Indian Ocean and rainfall in Africa and Australia.
Some trigger — Rossby waves reflecting off the western margin, the Madden - Julian Oscillation or something else — causes the winds to falter and
warm water flows east across the Pacific.
Warm water flows north and melts ice.
From 1964 there had been a constant increase in applied solar SW to the equatorial Atlantic (68 an exception) resulting in a constant stream of
warmer water flowing north along the E USA to artic.
Not exact matches
The reasons for this are many: less cold
water from Sierra snowpack, less cold freshwater being released from the Delta due to farming needs and other
water policies,
warm waters caused by El Nino
flowing into the Bay, and other variables.
The Kozii bottle / bag
warmer is designed specifically to thaw and
warm breastmilk using
warm,
flowing water... because when baby's hungry, a watch pot NEVER boils!
Wash your breasts and nipples with
warm water to remove any dried milk that may be obstructing the
flow of milk out of your breasts.
To get milk
flowing, many moms moms suggest taking a brief hot shower, putting a rice - filled sock in the microwave for a DIY
warm compress, and literally sticking your breasts in a sink filled with
warm water and massaging downward until a little milk comes out.
The
warm water seems to help get things
flowing, even after my son has already had his morning nursing.»
The device uses
flowing warm water to gently heat milk and food instead of boiling or steaming.
Baby will never get cold in this advanced bathtub as the entire system is designed to ensure a steady
flow of
warm, clean
water while effortlessly removing cold, dirty
water.
Its
warming method is based on
warm flowing water that surrounds the baby bottle and enables you to quickly thaw and
warms baby food and drink to safe temperatures.
Protect your liquid gold with the Kiinde Kozii, which safely thaws and / or
warms any bottle (and baby food pouches or jars) using a constant stream of
flowing water.
The
warm water increases blood
flow, which helps heal and repair damaged tissues in the area.
The
warm water can also increase blood
flow to the affected area and speed healing.
If milk in
flowing, take a hot shower to allow the
warm water to
flow over the engorged breasts.
The Kindii Kozii Bottle
Warmer makes use of the
flowing property of
water to create a
warm bath that in turn gently heats the bottle.
Likewise, increased milk
flow means increased production, so you'll want to avoid anything that causes your milk to
flow (like standing with your breasts under the
warm water in the shower).
When you turn the Kozii on, the bottle chamber fills and surrounds the bottle with
warm flowing water.
Extensive valley networks spidering through the southern highlands of Mars suggest that the planet was once
warmer and wetter, but new research shows that
water could still have
flowed intermittently on a cold and icy early Mars.
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.
It does so with a
warm flowing water bath.
By midsummer, low stream
flows and
warm water had killed half the annual sockeye salmon breeding run in the Columbia River.
The simulations suggest that over decades, these
warming events dramatically perturb the ocean surface, affecting the
flow of the Atlantic Meridional Overturning Circulation, a system of currents that acts like a conveyor belt moving
water around the planet.
If you decouple that ice from where it's grounded — something that currents of
warming water, already circulating around the Antarctic coast, could do — then
water could
flow beneath the inland ice and lubricate its slide into the ocean.
«The new data set will allow us to check if our ocean models can correctly represent changes in the
flow of
warm water under ice shelves,» he added.
The mystery of how
water on Mars lasted for millions of years may come down to methane explosions that
warmed the planet enough to melt ice and make rivers
flow
After further analysis of the data, the scientists found that although a strong El Niño changes wind patterns in West Antarctica in a way that promotes
flow of
warm ocean
waters towards the ice shelves to increase melting from below, it also increases snowfall particularly along the Amundsen Sea sector.
Today, as
warming waters caused by climate change
flow underneath the floating ice shelves in Pine Island Bay, the Antarctic Ice Sheet is once again at risk of losing mass from rapidly retreating glaciers.
«The closures are becoming an annual event when trout are stressed by
warm water and low
flows.
Warming in the 21st century reduced Colorado River
flows by at least 0.5 million acre - feet, about the amount of
water used by 2 million people for one year, according to new research from the University of Arizona and Colorado State University.
The Red Planet's thin atmosphere of carbon dioxide can't retain enough heat for
water to
flow on the planet, but new calculations suggest how it was once
warmer
Although today's Martian surface is barren, frozen and uninhabitable, a trail of evidence points to a once
warmer, wetter planet, where
water flowed freely.
As La Nia ends, the surface
water flows back and the coast is hit with unusually
warm water, which results in more rainfall.
Increased
flow of the East Australian Current, for example, has meant
waters south - east of the continent are
warming at two to three times the global average.
Overall, aquatic ecosystems in western North America are predicted to experience increasingly earlier snowmelt in the spring, reduced late spring and summer
flows,
warmer and drier summers, and increased
water temperatures — all of which spell increased hybridization between these species.
Because the way in which
water moves beneath ice sheets strongly affects ice
flow speeds, improved understanding of these lakes will allow us to predict more accurately how the ice sheet will respond to anticipated future
warming.»
«Hurricanes almost always form over ocean
water warmer than about 80 degrees F. in a belt of generally east - to - west
flow called the trade winds.
Around 11,000 years ago, as the last ice sheets retreated from Norway and the Norwegian Sea, Atlantic
water flowed in and
warmed the bottom by about 9 degrees Fahrenheit.
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.
The work has revealed previously unknown undersea channels, through which
warm water might
flow toward fragile ice shelves.