Sentences with phrase «warmer water temperatures also»

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 NoveWater 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 Novewater 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 sunliAlso, warmer temperatures alone in the boreal zone do not guarantee more plant growth, which also depends on the availability of water and sunlialso 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 tTemperature effects are also quite reliable, and are mainly for above normal temperature in and around the warmed oceanic waters in ttemperature 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.
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