Sentences with phrase «high sea level pressure»

Zhang, and W.R. Rossow, 2000: Cloud and radiation variations associated with northern midlatitude low and high sea level pressure regimes.

El Niño causes higher sea level pressure, warmer air temperature and warmer sea surface temperature in west Antarctica that affect sea ice distribution.

El Niño causes higher sea level pressure, warmer air temperature and warmer sea surface temperature in west Antarctica that affect sea ice distribution.

Not exact matches

Unrefined sea salt helps to regulate blood sugar, water content in our body and pH levels, help reduce high blood pressure, and actually contains less sodium than table salt.

Instead of weightlessness, the aquanaut would have to endure, among other things, artificial atmospheres with gaseous mixtures different from what we breathe on land, maintained at significantly higher pressures than those at sea level to match the water pressure at depth.

Blobfish live at depths of between 600 and 1,200 meters where the pressure is several dozen times higher than at sea level, and they can grow up to 12 inches in length.

The analysis of high - frequency surface air temperature, mean sea - level pressure, wind speed and direction and cloud - cover data from the solar eclipse of 20 March 2015 from the UK, Faroe Islands and Iceland, published today (Monday 22 August 2016), sheds new light on the phenomenon.

The sea level time series is rich in physical phenomena such as tides (caused mostly by the gravitational pull of the Moon and the Sun), meteorological signals (high and low pressure), and signals from climate change.

The higher sea level near the western ocean boundary creates a west - east pressure difference in the ocean, that results in the equatorial undercurrent flowing from west to east below the surface.

At altitudes of 5000 m and higher, life is not easy here: the atmospheric pressure is much lower than at sea level, and oxygen is scarce.

This is the result of adiabatic warming, where air is compressed from low pressure (at the top of a mountain) to high pressure (at sea level).

195º Low simmer 210º High simmer 212º Boiling water at sea level; light or vigorous boil 213º - 214º Boiling temperature of salted or sugared water; 1 teaspoon per quart 250º Maximum pressure cooker temperature 250º Butter smoke point 300º For seasoning lightly oil - coated pans in the oven 325º Water drops dance on skillet surface 325º Black pepper burning point 350º Clarified butter smoke point

Same as water boiling at sea level at 100C (212F) but at lower temp at high altitudes because pressure is less, same rule applies to refrigerant.

Patterns of anomalously high sea levels are attributed to El Niño — related changes to atmospheric pressure over the Gulf of Mexico and eastern Canada and to the wind field over the Northeast U.S. continental shelf.

Unlike the sea level pressure field from the last six years with the Arctic Dipole (AD), which has low pressure on the Siberian side of the Arctic and higher pressure on the North American side, May 2013 had a low pressure over the central Arctic.

So it sounds like even though at sea level freshwater at 4º or less does not expand when heated, that with the salinity and higher pressure, the deep ocean below 700m is actually expanding as it heats and thus adding a little to searise.

Radiation from the atmosphere's greenhouse gases is narrow - band, even at sea level but increasingly so at higher altitudes as the effect of pressure - broadening decreases.

In general, indices of the annular modes are based on either 1) the leading principal component (PC) time series of gridded geopotential height anomalies at a given pressure level or 2) approximations of the leading PC time series of geopotential height anomalies using differences between sea level pressure anomalies at stations in middle and high latitudes.

Bolin & Eriksson's «buffer» factor would give about 10 times higher CO2 concentration in air vs. sea water at about 0.0003 atmospheres CO2 partial pressure, increasing dramatically to an air / water CO2 partition coefficient of about 50:1 at a CO2 partial pressure of about 0.003 atmospheres (10 times the assumed pre-industrial level; Bacastow & Keeling, 1973; see Section 7 below for more on the «buffer» factor).

The increased west winds are related to lower sea level pressure at high latitudes, with greater sea level pressure in mid-latitudes.

The response pattern associated with GCR consisted of a negative temperature anomaly that was limited to parts of eastern Europe, and a weak anomaly in the sea - level pressure (SLP), but coincided with higher pressure over the Norwegian Ssea - level pressure (SLP), but coincided with higher pressure over the Norwegian SeaSea.

When solar activity is high — the sea level pressure at the poles is low and storms are constrained to a tight circle at high latitudes.

With regard to summer meteorological forcing, 2007 was dominated by a strong dipole pattern in sea level pressure (SLP), with high pressure over the Beaufort Sea and winds blowing from the Bering Strait across the North Pole, promoting both advection of warm air and compaction of the ice pasea level pressure (SLP), with high pressure over the Beaufort Sea and winds blowing from the Bering Strait across the North Pole, promoting both advection of warm air and compaction of the ice paSea and winds blowing from the Bering Strait across the North Pole, promoting both advection of warm air and compaction of the ice pack.

Sea level pressures continued to be predominantly high in the central Arctic through July and early August (Figure 7).

High storm surges (sea levels raised by storm winds and atmospheric pressure) also tend to move coastal sand offshore.

The cooling increases polar sea level pressure pushing the storms circling the pole into higher latitudes.

In a positive SAM event sea level pressure over the pole is relatively low and pressure at sub-polar regions relatively high.

1 g / kg has a partial pressure of 0.001 * p / 0.622 which is 1.6 mb at sea level, less higher up.

Sea - level pressure over the Arctic Ocean has tended to be fairly high, while pressure has been fairly low over northeastern Siberia.

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A persistent ridge of higher than normal sea level pressure was present over the Gulf of Alaska from October 2013 into February 2014.

The Arctic had a weak Dipole Sea Level Pressure (SLP) with a low on the Eurasian Side and a high pressure region from north of the Bering Strait across northern Canada; the SLP pattern is typical of the long term average (1981 Pressure (SLP) with a low on the Eurasian Side and a high pressure region from north of the Bering Strait across northern Canada; the SLP pattern is typical of the long term average (1981 pressure region from north of the Bering Strait across northern Canada; the SLP pattern is typical of the long term average (1981 - 2010).

Figure 1 (below) is the sea level pressure field for June and July 2009, showing the Dipole / negative Arctic Oscillation pattern with high pressure on the North American side of the Arctic.

Prior to vortex displacements the main sea level pressure anomaly center of the tropospheric precursor is associated with the Siberian high.

Average sea level pressure is 29.92 inches (1013.23 mb), making this record pressure 7 % higher than normal, which means there was 7 % more atmospheric mass above that point than normal.

Previous theoretical and model - based studies of the relationship between ocean bottom pressure (pb) and sea level (ζ) suggest primarily barotropic variability at mid to high latitudes for scales greater than a few hundred kilometers and periods less than a few months.

Since May, sea - level pressure anomalies over northern Australia have been persistently high, while pressure anomalies over the tropical eastern Pacific have been mostly lower than average.

Even if the statistical relationship is valid, EJN's physical interpretation is faulty: a westward and southward shift of the Bermuda High causes an increased meridional sea level pressure gradient and stronger tradewinds over the main development region, not a relaxation of the tradewinds.

The map of sea level pressure for October 1 to 30, 2010, shows a high - pressure system cenetered over the Beaufort and Chukchi sea and Greenland, and low pressure over the Kara and Barents seas.

Therefore, by computing (or measuring) the absorption at sea level pressure, we are overestimating the absorption of the CO2 actually in place in the higher, lower - pressure parts of the atmosphere.

Lukovich et al. (Centre for Earth Observation Science, U. of Manitoba); 4.4 to 4.5; Heuristic - Dynamics The absence of a strong and persistent sea level pressure high over the Beaufort in July together with the absence of spatial homogeneity in the springtime sea ice drift fields suggest that continued sea ice decline will be an artifact of increased temperatures and thermodynamic forcing rather than the considerable dynamical contributions seen in summer of 2007.

Holds the high correlation among the variables composing these changes — temperature, precipitation, cloudiness, sea level pressure (SLP), and ice concentration — suggests that their close coupling collectively represents a fingerprint of Arctic climate change

While the DA was replaced by low sea level pressure (SLP) over the Arctic Ocean in July, high pressure returned over the Beaufort Sea in August coupled with low pressure over Siberia, helping to compress ice towards the pole and bring warm air into the Arctsea level pressure (SLP) over the Arctic Ocean in July, high pressure returned over the Beaufort Sea in August coupled with low pressure over Siberia, helping to compress ice towards the pole and bring warm air into the ArctSea in August coupled with low pressure over Siberia, helping to compress ice towards the pole and bring warm air into the Arctic.

By 2050, he said, the triple pressures of growing population, economic development, and higher irrigation needs due to a warming climate will increase that to 0.82 millimeters per year — enough to raise sea levels by 40 millimeters (1.6 inches) above 1990 levels.

However, during the second half of July, ice loss slowed substantially as the high pressure over the central Arctic and Beaufort Sea was replaced by low sea level pressure (Figure Sea was replaced by low sea level pressure (Figure sea level pressure (Figure 3).

Hence, CO2 and water vapor must, in an equilibrium, produce about 33 ° C. However, at the top of Everest the temperature in the high summer climbing season is about -16 and in winters falls to about -37 ° C, yet the CO2 pressure is only about a third of that at sea level.

For stratospheric circulation (which impacts strat - trop exchange, high latitude sea level pressure fields), we tune the GW drag.