They spend
winters near the surface, and they are one of the first species to come out when things thaw.
Got a question for model experts about
winter near surface inversions.
Not exact matches
The researchers found that when Arctic warming occurred
near the
surface, the connection to severe
winter weather was weak.
Wings also operate under drier conditions when they're at altitude; turbine blades
near the
surface are in the middle of
winter sleet and snow.
They also looked at recent ocean conditions, in particular the temperature of the sea
surface near Japan and Florida the
winter before a given breeding season.
Suck up
near - freezing water from under the ice and pump it directly onto the ice's
surface during the long polar
winter.
Pirelli's Temperature Dynamic Compound technology optimizes the compounds for wet and icy
surfaces to provide improved traction in
winter's
near freezing and lower temperatures.
They are sexually mature at 3 - 8 years of age; they breed every 2 years in late
winter to early spring in warmer waters
near the
surface.
17 El Nino verses La Nina El Niño La Niña Trade winds weaken Warm ocean water replaces offshore cold water
near South America Irregular intervals of three to seven years Wetter than average
winters in NC La Niña Normal conditions between El Nino events When
surface temperatures in the eastern Pacific are colder than average The southern US is usually warmer and dryer in climate
«As
winter sets in, lakes lose energy to the atmosphere, and water
near the
surface cools, becomes more dense, and sinks.
The implication is that summer temperatures predispose the
near -
surface waters to above - or below - normal ice coverage in the following fall and
winter.
The predictor is
winter (Jan - Feb - Mar)
near global sea
surface temperature.
Using a statistical model based on
winter near - global sea
surface temperatures, Tivy shows high concentrations of ice remaining throughout the NWP region.
The forecast possibility of El Niño
nears 50 % by the
winter, as many of the computer models are trending to warmer tropical sea
surface conditions in the later months of 2018.
For example, in the caption to Fig. 6: «Tmax is, as expected, lower on windy than on calm days in summer (b), but higher on windy than on calm days in
winter (a), because persistent
near -
surface inversions are limited to calm weather.»
The
near -
surface temperature anomalies [degrees C], relative to a 1981 - 2010 base period from NCEP - NCAR reanalysis, averaged over November - March for (left) La Niña
winters without any SSWs, (middle) La Niña
winters with at least one SSW, and (right) observed conditions in 2017 - 18.
First, that the oceanographers are correct in their present hypothesis, that a persistent failure of late
winter sinking of the ocean
surface near Greenland and Iceland is a likely cause of most of the abrupt cooling episodes.
Winter mixing brings nutrients up from below, concentrating them
near the
surface.
The lapse rate (despite the temperature inversions
near the
surface at night and in the
winter polar regions) insures that the radiation of the air absorbed by the
surface is slightly less than the radiation of the
surface absorbed by the air.
Finds that the largest single determinant of the
near -
surface freshwater percentages is found to be changes in mixed layer depth — notably deep layers occurred in the
winters of 2003, 2007 and 2008, due to northerly winds associated with El Niño / Southern Oscillation and the Southern Annular Mode
These take advantage of the remarkable stability of the earth's temperature
near the
surface and then use that as a source of heat in the
winter when the air temperature is low and a source of cooling in the summer when the temperature is high.
During a dry
winter, the reduction of aerosol concentrations in weekend days may overwhelmingly impact on the DTR through a direct effect, i.e. by increasing total solar irradiance
near the
surface and raising the daytime temperature and maximum temperature, and lowering relative humidity.
Irrigation also leads to boreal
winter (December - February) warming over parts of North America and Asia in the latter part of the century, due to enhanced downward longwave fluxes from increased
near surface humidity.