Sentences with phrase «between equatorial»

Biophysical Mechanisms and Feedbacks Defining the Boundaries of the Closed - Canopy Equatorial Forest At the continental scale, nonlinear feedbacks between the equatorial forest and the atmosphere have been recognized for decades.

One of the biggest differences between equatorial deserts and jungles is that the lapse rate in the desert is steep because it's close to the dry adiabatic rate.

With an evident relationship across the CMIP5 models between equatorial SSTs and upper ocean temperatures in the extra-tropical subduction regions, our analysis suggests that cold SST biases within the extra-tropical Pacific indeed translate into a cold equatorial bias via the STCs.

Schneider, E.K., 2001: Causes of differences between the equatorial Pacific as simulated by two coupled GCM's.

The game between Equatorial Guinea and Congo will be followed by Burkina Faso vs. Gabon (7 pm), which will also be live on Eurosport.

Mauritian referee Rajindraparsad Seechurn has been slapped with a six - month ban after he was at the centre of controversy during this weekend's game between Equatorial Guinea and Tunisia, the Metro reports.

Not exact matches

Such conditions are found around the world in locations along the Equatorial zone, between latitudes 25 degrees North and 30 degrees South.

CHAN 2018: The match between Super Eagles of Nigeria and Equatorial Guinea ended with Nigeria scoring 3 - 1 in the evening of Tuesday.

Their data showed that the difference between polar and equatorial sea surface temperatures in the Eocene was an estimated 20 degrees Celsius, about 36 degrees Fahrenheit.

The results indicate that glaciers in equatorial East Africa advanced between 24,000 and 20,000 years ago at the coldest time of the world's last ice age.

It is possible, he adds, that these persistent high - pressure zones may be produced by two well - known oceanographic patterns: La Nina and El Nino in the Pacific Ocean (which mark alterations in warmer and cooler conditions between that ocean's eastern and western equatorial waters) and the North Atlantic Oscillation (which results from weather patterns between Iceland and the Azores).

Researchers analyzed fossilized pollen and carbon isotopes in New Mexico rock layers to reconstruct the equatorial climate between 205 million and 215 million years ago.

Equatorial crossings are determined by two numbers: the position on the equator (longitude), and the angle between the geodesic and the equator.

Interestingly, it shows a prominent equatorial dark lane sandwiched between two brighter features, due to relatively low temperature and high optical depth near the disk midplane.

Earth's surface may have froze mostly or thinly solid through equatorial regions (see debate between the «Snowball» versus «Slushball» Earth hypotheses).

Tropical rainforest A tropical rainforest is an ecosystem type that occurs roughly within the latitudes 28 degrees north or south of the equator (in the equatorial zone between the Tropic of Cancer and Tropic of Capricorn).

For example, in Earth atmospheric circulation (such as Hadley cells) transport heat between the warmer equatorial regions to the cool polar regions and this circulation pattern not only determines the temperature distribution, but also sets which regions on Earth are dry or rainy and how clouds form over the planet.

A tropical rainforest is an ecosystem type that occurs roughly within the latitudes 28 degrees north or south of the equator (in the equatorial zone between the Tropic of Cancer and Tropic of Capricorn).

Changes in climate can cause the polar jet stream — the boundary between the cold North Pole air and the warm equatorial air — to migrate south, bringing with it cold, Arctic air.

In the early 1990s, one study found that coplanarity between the orbital and equatorial planes of nearby binaries (within 100 parsecs or 326 ly) that are composed of Sol - type stars (F5 - K5 V) «exists» for binaries with orbital separations up to the average orbital distance of Pluto in the Solar System — roughly 40 times the Earth - Sun distance or «astronomical unit» (AU).

7 During the winter, the Marine Bio Conservation Society states that the gray whales inhabit shallow coastal waters of the eastern and western North Pacific often sighted along the North American Pacific Coast between the arctic and the equatorial lagoons of Baja California, Mexico.

A measure of the difference in sea level pressure between the western (e.g., Darwin, Australia) and central / eastern (e.g., Tahiti) equatorial Pacific, representative of the east - west changes in atmospheric circulation associated with the El Nino / Southern Oscillation phenomenon.

SA13A - 2269: Relationship between lunar tidal enhancements in the equatorial electrojet and tropospheric eddy heat flux during stratospheric sudden warmings

The climate in equatorial east Africa has alternated between drier than today, and relatively wet.

ENSO is often measured by the difference in surface pressure anomalies between Tahiti and Darwin and the SSTs in the central and eastern equatorial Pacific.

Furthermore, possible connections between the new transport time series of the North Brazil Undercurrent (NBUC) and the transport variability of the Equatorial Undercurrent (EUC) as well as the resulting consequences for the climate relevant surface temperatures of the equatorial East Atlantic will beEquatorial Undercurrent (EUC) as well as the resulting consequences for the climate relevant surface temperatures of the equatorial East Atlantic will beequatorial East Atlantic will be analyzed.

The CESM experiments reveal a quadratic relationship between extra-tropical Pacific albedo and the root - mean - square - error in equatorial SSTs — a relationship with which the CMIP5 models generally agree.

Interactions between externally - forced climate signals from sunspot peaks and the internally - generated Pacific Decadal and North Atlantic Oscillations «When the PDO is in phase with the 11 year sunspot cycle there are positive SLP anomalies in the Gulf of Alaska, nearly no anomalous zonal SLP gradient across the equatorial Pacific, and a mix of small positive and negative SST anomalies there.

Equatorial Countercurrent — between the westward warm equatorial currents of the Atlantic, Pacific, and IndiEquatorial Countercurrent — between the westward warm equatorial currents of the Atlantic, Pacific, and Indiequatorial currents of the Atlantic, Pacific, and Indian Oceans.

It is often measured by the surface pressure anomaly difference between Darwin and Tahiti and the sea surface temperatures in the central and eastern equatorial Pacific.

The Zhang & McPhadden papers do indeed highlight the spin - down and then spin - up of the wind - driven ocean circulation, but one place to start is: Interaction between the Subtropical and Equatorial Ocean Circulations: The Subtropical Cell -(McCreary & Lu 1994).

The difference between the GRIP core and the Tierney or other equatorial core, would give you you a reasonable estimate of the maximum rate of internal heat transfer.

«The authors write that «the El Niño - Southern Oscillation (ENSO) is a naturally occurring fluctuation,» whereby «on a timescale of two to seven years, the eastern equatorial Pacific climate varies between anomalously cold (La Niña) and warm (El Niño) conditions,» and that «these swings in temperature are accompanied by changes in the structure of the subsurface ocean, variability in the strength of the equatorial easterly trade winds, shifts in the position of atmospheric convection, and global teleconnection patterns associated with these changes that lead to variations in rainfall and weather patterns in many parts of the world,» which end up affecting «ecosystems, agriculture, freshwater supplies, hurricanes and other severe weather events worldwide.»»

The QBO in WACCM4 is prescribed by relaxing equatorial zonal winds between 86 and 4 hPa to observed radiosonde data (28 - month period).

The trade winds are driven by the SST differences between the Pacific Warm Pool and the Eastern Equatorial Pacific, and vice versa.

The average annual SST difference between the east and west equatorial Pacific is about 4.5 deg C. Refer to the graph I prepared for an upcoming post.

The equatorial Pacific alternates between warm and cool surface temperatures as El Niño or La Niña.

I see no correlation between the solar cycles and equatorial temperatures at 20hPa and 200hPa.

Between the two equatorial currents driven by the trade winds is the equatorial counter-current.

It guides the movement of mid latitude depressions and effectively marks an interface between warmer equatorial air and colder polar air.

Yu, J. - Y., and C. R. Mechoso, 1999: Links between annual variations of Peruvian stratus clouds and of SST in the eastern equatorial Pacific.

In general, when data differences between two satellites were found, a decision was made as to which satellite was correct and which was in error, based on local equatorial crossing time variations or other factors.

between these two events it appeared that they altered the Azores high sufficient to move the ITCZ about 1 degree north, thus producing a temporary increase in EWSC over the equatorial Atlantic sufficient to cause a net relative cooling.

As explained by MIT physicist Richard Lindzen, the reduction of the temperature differential between the north hemisphere and the equatorial part of our planet makes cyclonic energy much smaller: the importance and frequency of extreme events thus tend to decrease.

Create a temperature profile for high, medium and equatorial latitudes and you can imagine that during glacial periods there is less variation between the deep and shallow layers.