All other environmental variables tested, including the UI (from April to September only), the PDO, silicate, nitrate and
the seawater temperature at Tatoosh, were not associated with shell δ13C (Table 2).
It also caused a decrease in precipitation by approximately 70 - 85 percent on land and a decrease of approximately 5 - 7 °C in
seawater temperature at a 50 - m water depth, leading to mass extinction of life forms including dinosaurs and ammonites.
Not exact matches
The ratio of oxygen isotopes in
seawater depends on the water
temperature; the value of this ratio
at any point in evolutionary time is «frozen» into the chemical composition of certain marine fossils.
The results show that blue crabs can —
at moderate water
temperatures — survive
at oxygen levels as low as 1.3 milligrams per liter, just 15 % of the oxygen available in fully saturated
seawater.
The Calera process essentially mimics marine cement, which is produced by coral when making their shells and reefs, taking the calcium and magnesium in
seawater and using it to form carbonates
at normal
temperatures and pressures.
In the study, published in the journal Proceedings of the Royal Society B: Biological Sciences, researchers
at the UC Davis Bodega Marine Laboratory raised bryozoans, also known as «moss animals,» in
seawater tanks and exposed them to various levels of water
temperature, food and acidity.
The increase could be due to a combination of stronger winds spreading out the sea ice and fresh water from melting ice on land diluting
seawater so it freezes
at higher
temperatures.
Most Antarctic researchers chalk this up to warm
seawater melting the floating ice shelves
at their bases;
seawater temperatures there have risen since the 1970s, in part because of global
temperature increases.
When
seawater freezes it expels its salts, producing a layer of very dense, briny water
at the freezing
temperature.
Microbial communities in
seawater from an Arctic and a temperate Norwegian fjord and their potentials for biodegradation of chemically dispersed oil
at low
seawater temperatures — Deni Ribicic — Marine Pollution Bulletin
The researchers analysed resting and active jumping oxygen consumption rates in snails exposed to
seawater at the normal
temperature of 29 °C and
at the increased
temperature of 34 °C, projected to be reached during the next 100 years due to global warming.
They were able to maintain this strong increase in oxygen uptake even when the
seawater temperature was increased to 37 °C — a
temperature at which coral reef fish can not even survive for a short time.»
«We knew that the environment was harsh, with -20 Celsius -LSB--4 degrees F] air
temperatures and sea
temperatures very close to the freezing point of
seawater,» said Steve McPhail, head of AUV Development
at the NOC, in a statement.
The facility has an 18,000 gal recirculating
seawater system which supplies tanks in both indoor and semi-enclosed outdoor spaces with a constant supply of clean water
at local environmental
temperatures.
Maybe Trenberth thought our observations lacked a few data points, for example
at the time he wrote that email, the observational evidence for
seawater temperatures below 700 meters was, shall we say scant.
The open cycle consists of the following steps: (i) flash evaporation of a fraction of the warm
seawater by reduction of pressure below the saturation value corresponding to its
temperature (ii) expansion of the vapor through a turbine to generate power; (iii) heat transfer to the cold
seawater thermal sink resulting in condensation of the working fluid; and (iv) compression of the non-condensable gases (air released from the
seawater streams
at the low operating pressure) to pressures required to discharge them from the system.
That may seem small
at first, but over time, especially when combined with other sources of sea level rise such as melting Greenland glaciers and the expansion of
seawater as ocean
temperatures increase, it adds up.
Instrumental data on
seawater temperature, salinity, pH, dissolved oxygen, and chl a have been recorded every 30 min during the spring and summer months since 2000
at Tatoosh Island.
At first, the
seawater was sampled using a bucket, hauling it onto the ship's deck and measuring the water
temperature with a thermometer.
Explanations for this have included physiological barriers, an example being the decapod crustaceans, which have an inability to down - regulate blood magnesium levels sufficiently below that of
seawater, leading to a loss of activity and eventual death
at polar water
temperatures [57].
The rest of the 100 + ppmv (80 ppmv since the measurements
at the South Pole started) is NOT from the
seawater temperature increase.
Even zero - degree
seawater at outer continen tal shelf depths could expose ice shelves with deep grounding lines like the Totten (2.2 km), Moscow (2.0 km) and Shackleton (1.8 km) to
temperatures more than 3 °C above their melting points.»
For the long - term experiment, the constant
temperature regimes of the
seawater bath were replaced with a seasonal cycle (adjusted monthly; see electronic supplementary material, figure S2) to match either historical mean monthly
temperatures at the study site (ambient) or a warming scenario (ambient cycle +4 °C).
Aquaria in the short - term experiment were held in a
seawater bath
at a constant
temperature (Titan 1500 chiller unit, Aqua Medic) to reflect either the annual mean
temperature of the study site (10.24 ± 0.02 °C; see electronic supplementary material, figure S2) or a warming scenario of +4 °C (14.36 ± 0.12 °C; see electronic supplementary material, figure S2).
Radiation from a molecule
at -80 C therefore can not provide enough energy in the form of photons, to warm molecules (by boosting electrons into higher, more energetic orbits)
at -4 C or above (
seawater temperatures).