But
warmer water temperatures also mean warmer fish — and faster - running metabolisms.
Not exact matches
I
also cut my recipe in half as it makes quite a lot, this is the whole recipe: 3 1/4 - 4 cups plain flour 1 1/2 cups chilled unsalted butter 2 packages active dry yeast (4 1/2 tsp) 1/2 cup
warm water 1/2 cup heavy cream or undiluted evaporated milk 1/2 tsp freshly crushed cardamom seed (optional) 1/2 tsp salt 2 eggs, room
temperature 1/4 cup sugar Directions would be the same as mine but start off with 3 1/2 cups of flour and add the eggs with the cream.
It is
also much faster and more economical than
warming water in a pot or kettle and waiting for it to get the right
temperature before placing the bottle inside.
You
also can put your baby's bottles in a pan of
warm water (away from the heat of the stove) and then test the
temperature by squirting a drop or two on the inside of your wrist before feeding your baby.
The soft TPE plastic does not only mould comfortably around your baby, but
also takes up the bath
water's
temperature very quickly, which makes your baby feel
warm and safe.
It's
also thick enough to keep you
warm and comfortable in any
water temperature.
The data
also show a land bump, or sill, at the mouth of Skinfaxe glacier, which prevents
warmer, deep Atlantic
water (yellow on
temperature bar) from reaching the ice.
His discoveries have
also revealed how
warming ocean
temperatures and acidification of ocean
water caused by climate change lead to coral bleaching and death.
Warmer temperatures also would transform the environment of the San Francisco Bay and Sacramento - San Joaquin Delta, a system that provides
water for 25 million people and irrigates $ 36 billion in annual crops.
Taylor and her colleagues
also tested
water temperature and pH levels in the laboratory to study the impact of ocean
warming and acidification on the exoskeletons of several species of crustacean.
Besides shrinking in extent, the sea ice cap is
also thinning and becoming more vulnerable to the action of ocean
waters, winds and
warmer temperatures.
Scientists were
also surprised to find that the reef in Tanzania was able to adapt to
warmer water temperatures.
Invasions are
also more likely if the start point is in
warm water, which usually contains more species, and if the
water at both ports is of similar
temperature and salinity.
With higher levels of carbon dioxide and higher average
temperatures, the oceans» surface
waters warm and sea ice disappears, and the marine world will see increased stratification, intense nutrient trapping in the deep Southern Ocean (
also known as the Antarctic Ocean) and nutrition starvation in the other oceans.
«But if this study is correct, we should
also expect average
water supply for humans to decline over the long term as
temperatures warm.»
Not only does the ChiliPad allow you to control your
temperature, but it
also provides all - night relief, works with your existing mattress and evenly distributes your desired
temperature throughout your bed with
water - cooling and
warming technology.
Not only does the ChiliPad allow you to control your
temperature, but it
also provides all night relief, works with your existing mattress and evenly distributes your desired
temperature throughout your bed with
water - cooling /
warming technology.
For pets with sensitive skin or skin disease we
also recommend bathing with luke -
warm to slightly cool
water temperature, because heat can intensify the sensation of itch.
Your pet's body
temperature is
also maintained by the use of a circulating
warm water pad.
Water temperatures also vary greatly from a cool chilly May and June where water can dip to the high 50's (15 c) to a warm and tropical mid 80's (30 c) from September to Nove
Water temperatures also vary greatly from a cool chilly May and June where
water can dip to the high 50's (15 c) to a warm and tropical mid 80's (30 c) from September to Nove
water can dip to the high 50's (15 c) to a
warm and tropical mid 80's (30 c) from September to November.
Because of Lanzarote's year - round
warm temperatures, the average sea
temperature for the
waters around the island is
also mild throughout the year, especially in June when it's 21 °C.
With
water temperatures ranging between 24 and 28 °C, it is often a little
warmer in Sangeang than in Komodo National Park, where you will
also likely be diving.
Long continuous records of
temperature and salinity at Ocean Weather Station M in the Norwegian Sea indicate that the deep
water has
also warmed noticeably.
... Increases in
temperatures of the higher latitudes would
also decrease density because
warmer water is less dense.
It
also seems that even though the selective absorption of specific energy bands by different molecules IS the mechanism to add energy to the air, the energy absorbed by CO2 & especially
Water Vapor is extremely rapidly dispersed by molecular collisions to ALL the components of the atmosphere, so that the N2 and O2
also heatup, and all the atmospheric components assume a uniform
temperature (ie global
warming).
The structure of the ocean circulation basically anchors this region to something like pre-industrial
temperatures, at least until deep bottom
water originating in the North Atlantic
also warms.
In the tropics which are prone to deep convection, the
water vapor response to
warmer temperature also promotes a less steep lapse rate owing to latent heat effects.
The vertical
temperature profile may
also play a role, as
warmer water is lighter, and thus the stability of the
water column depends on how fast the
temperature drops with depth — more stable
water column is less prone to mixing.
Also, warmer temperatures alone in the boreal zone do not guarantee more plant growth, which also depends on the availability of water and sunli
Also,
warmer temperatures alone in the boreal zone do not guarantee more plant growth, which
also depends on the availability of water and sunli
also depends on the availability of
water and sunlight.
The resulting weaker density stratification allowed more vertical mixing of the
water column during storms in late September and early October, leading to the observed
warming of the near - bottom layer in the still ice - free Laptev Sea...
Warmer water temperatures near the seabed may
also impact the stability of the shelf's submarine permafrost.»
Scientists
also know that freshwater
temperatures are rising because
warm -
water species are moving into areas that were formerly too cold, while cool - and cold -
water species are likewise on the move.
East Coast winter storms, known as «nor» easters» because of the unusual northeasterly direction of the winds as the storm spirals in from the south, are unusual in that they derive their energy not just from large contrasts in
temperature that drive most extratropical storm systems, but
also from the energy released when
water evaporates from the (relatively
warm) ocean surface into the atmosphere.
Also at New York Times (though what to make of «scientists said the ice sheet was not melting because of
warmer air
temperatures, but rather because of the relatively
warm water, which is naturally occurring, from the ocean depths»...?)
Temperature effects are also quite reliable, and are mainly for above normal temperature in and around the warmed oceanic waters in t
Temperature effects are
also quite reliable, and are mainly for above normal
temperature in and around the warmed oceanic waters in t
temperature in and around the
warmed oceanic
waters in the Pacific.
This could lead to agricultural drought and suppressed crop yields.15 This would
also increase thermoelectric power plant cooling
water temperatures and decrease cooling efficiency and plant capacity because of the need to avoid discharging excessively
warm water (see
also Ch.
Scientists
also know that ocean
temperatures are rising because
warm -
water species are moving into areas that were formerly too cold, while cool -
water and cold -
water species are likewise on the move.
This can be affected by
warming temperatures, but
also by changes in snowfall, increases in solar radiation absorption due to a decrease in cloud cover, and increases in the
water vapor content of air near the earth's surface.2, 14,15,16,17 In Cordillera Blanca, Peru, for example, one study of glacier retreat between 1930 and 1950 linked the retreat to a decline in cloud cover and precipitation.18
The
water vapor within the brick is
also at a
warmer temperature than its surroundings.
The IPCC most certainly
also claims
water vapour
warms, doing most of «33 degrees» of
warming, whereas, in fact, it cools the surface by reducing the
temperature gradient whilst still keeping radiative balance with the Sun.
But Trenberth, suspecting that global
warming was
also playing a role, looked beyond the Atlantic to
temperature patterns throughout Earth's tropical and midlatitude
waters.
In addition,
warmer waters are pouring in from rivers in rapidly
warming land regions of Alaska, Canada, and Russia,
also increasing sea
temperatures.
While a negative AO leads to
warmer temperatures over the Arctic, it
also tends to reduce the flow of sea ice out of the Arctic by affecting the winds that can export the ice to
warmer waters, where it melts.
The location of Iceland with respect to the North Atlantic Drift, which carries
warm water from the tropics towards the poles, may
also contribute to the
temperature series being mismatched with records from Greenland or Scotland.
In addition to rising
temperatures, the report discussed a variety of «other possible effects of an increase in atmospheric carbon dioxide», including melting of the Antarctic ice cap, rise of sea level,
warming of sea
water, increased acidity of fresh
waters (which
also applies to the danger of ocean acidification, global
warming's evil twin), and an increase in plant photosynthesis.
«The dramatic changes in lake ice may
also contribute to further
warming of the entire region, because open
water on lakes contributes to
warmer air
temperatures, albeit to a lesser extent than open seawater,» Surdu said.
In cold or snow - dominated river basins, atmospheric
temperature increases do not only affect freshwater ecosystems via the
warming of
water (see Chapter 4) but
also by causing
water - flow alterations.
Surely these differences would be more significant if some showed cooling, other Global
temperature measurements such as Radiosonde, SST's and the proxy atmospheric
water vapor
also indicate
warming, so inconsistancies between the indexs surel are more a technical issue.
Another fact she ignores and one which is
also based on the density relationship to
temperature: Cold
water forcefully DISPLACES
warmer water upward.
For example, reductions in seasonal sea ice cover and higher surface
temperatures may open up new habitat in polar regions for some important fish species, such as cod, herring, and pollock.128 However, continued presence of cold bottom -
water temperatures on the Alaskan continental shelf could limit northward migration into the northern Bering Sea and Chukchi Sea off northwestern Alaska.129, 130 In addition,
warming may cause reductions in the abundance of some species, such as pollock, in their current ranges in the Bering Sea131and reduce the health of juvenile sockeye salmon, potentially resulting in decreased overwinter survival.132 If ocean
warming continues, it is unlikely that current fishing pressure on pollock can be sustained.133 Higher
temperatures are
also likely to increase the frequency of early Chinook salmon migrations, making management of the fishery by multiple user groups more challenging.134
«With global
temperatures warmer now than they were at the beginning of the last century, that means our
temperatures are
warmer too, which increases the rate of evaporation and increases the demands on
water, increases the stress on the
water supply, and
also leaves us more susceptible to breaking the high -
temperature record, which we've been doing lately,» Nielsen - Gammon said.