troposphere

The pressure at the top of the troposphere is only 10% of that at sea level and above this layer the pressure continues to drop.

The troposphere is the human home. We live directly in the bottom of the troposphere, and all weather phenomenon takes place on story here.

At the beginning of the 20th century, Nikola Tesla proposed using huge coils to transmit electricity through the troposphere to power homes.

The line between the troposphere and the rest of the blue-colored atmosphere is called the tropopause.

From the outside in the sun for a nuclear reaction zone, the troposphere the sun, the sun's atmosphere.

The orange layer is known as the troposphere, where all of the weather and clouds are generated and contained.

The stratosphere begins about 12 kilometres up, above the troposphere where weather systems like the monsoon develop.

As a rule, the temperature in the troposphere decreases steadily with increasing altitude until the tropopause is reached.

The OH radical initiated degradation of ethane was possibly one of the main sources of H2O2, MHP and EHP in the troposphere.

The rest is in the stratosphere, from the top of the troposphere to an altitude of 50 kilometers.

Can the dynamical impact of the stratosphere on the troposphere be described by large-scale adjustment to the stratospheric PV distribution?

When they re-enter the troposphere, they are rapidly washed out of the atmosphere by rain and snow.

The balance must be made up by heat transported through the troposphere.

Latent heat release accompanying deep convection is critical in offsetting longwave radiative cooling in the middle and upper troposphere.

STE may affect climate by altering the vertical distributions of greenhouse gases in the upper troposphere and low stratosphere.

The enhancement of moisture flux convergence in lower layers of troposphere is a favorable condition for rainfall in Northeast China.

Above the troposphere is the stratosphere, followed by the ionosphere and capped by the exosphere.

during the sand - dust storm , the high pv spreads evidently downward from the upper troposphere.

the resulting colder stratosphere emits less long-wave radiation downward, thus cooling the troposphere.

Troposphere the lowest level in the atmosphere, close to the Earth's surface, the thickness of approximately 10-20 kilometres.

Space transitions into the orange-colored troposphere, the lowest portion of Earth's atmosphere.

N, respectively. Thus, the zonal mean wind was weakened in the upper troposphere and the stratosphere over the region about 60?

Rossby Wave Breaking in the Southern Hemisphere Wintertime Upper Troposphere.

Besides, the planetary monsoon in the upper troposphere is also realistically reproduced.

Water Vapor Feedback in the Tropical Upper Troposphere: Model Results and Observations.

The role of heterogeneous reactions and procedure in the troposphere are assessed strictly.

The troposphere is a rich soup of oxygen rich air. It is unstable, chaotic, and unpredictable. but life depends upon it.

In summertime this dipolar pattern weakens to great extent and limits in the bound of troposphere.

There is strong evidence that vigorous narrow current is observed in the upper troposphere and stratosphere.

Winter and spring to the upper troposphere, almost no water vapor.

HF ultimately diffuses down to the troposphere where it is removed by wet deposition.

In the ENSO cold phase, because the Siberian ridge in upper troposphere strengthens, the Siberian high strengthens in lower troposphere.

Hopflied troposphere model and accurate troposphere model in radio wave refraction error modify in troposphere are gived.

The dynamic response to the heating imbalance is such as to converge heat into the upper troposphere of the desert regions.

Because of the above reasons stratospheric more easily than the troposphere by chemical pollution.

Above the troposphere, some 30 miles (48 kilometers) above the Earth's surface, is the stratosphere.

About 10 percent of ozone is in the troposphere, from the Earth's surface upward 10 kilometers to 16 kilometers.

The pollutants such as nuclear explosions, in the stratosphere than in the troposphere lot more.

A Simulation Study of Stratosphere-Troposphere Exchange due to Cut-off-low over Eastern Asia

Persistence of a Kelvin-Helmholtz instability complex in the upper troposphere

Modelling the effects of mixing processes on the composition of the free troposphere using a three-dimensional chemical transport model

A case study of stratosphere-troposphere exchange during the 1996 North Atlantic Regional Experiment

The Mean-Meridional Transport Circulation of the Troposphere in an Idealized GCM

Stratosphere-troposphere evolution during polar vortex intensification

Study on the System for Implementation of OTH Radar Signal Reconnaissance by Using Troposphere Scattering

Modeling atmospheric stable water isotopes and the potential for constraining cloud processes and stratosphere-troposphere water exchange

Relationship Between Vertical Shear of Zonal Wind in Equatorial Lower Stratosphere and Troposphere Circulation, Monsoon

First Regional Observing Study of the Troposphere;

Large horizontal gradients in atmospheric CO at the synoptic scale as seen by spaceborne Measurements of Pollution in the Troposphere

Regional and global trace gas distributions and inferred transports in the upper troposphere and lower stratosphere

Diurnal cycle of convection, clouds, and water vapor in the tropical upper troposphere: Satellites versus a general circulation model

Antarctic mesospheric temperature estimation using the Davis mesosphere-stratosphere-troposphere radar

Evidence of significant large-scale impacts of boreal fires on ozone levels in the midlatitude Northern Hemisphere free troposphere

Air masses and aerosols chemical components in the free troposphere at the subtropical northeast atlantic region

Key Technology of the New Generation Troposphere Scatter Communication System

Atmospheric chemistry of formaldehyde in the Arctic troposphere at Polar Sunrise, and the influence of the snowpack

Diagnosing the stratosphere-to-troposphere flux of ozone in a chemistry transport model

Improving the calculation of particle trajectories in the extra-tropical troposphere using standard NCEP fields

Signatures of stratosphere to troposphere transport near deep convective events in the southern subtropics

Simulation of Stratosphere-Troposphere Exchange Effecting on the Distribution of Ozone over Eastern Asia

Deposition ice nucleation on soot at temperatures relevant for the lower troposphere

Guided propagation of naturally occurring infrasound in the troposphere and stratosphere

Mean radiative energy balance and vertical mass fluxes in the equatorial upper troposphere and lower stratosphere

Structure Constant Model of Troposphere Atmosphere Turbulence on Microwave Slant-Paths

Transfer of the solar signal from the stratosphere to the troposphere: Northern winter

Airborne measurements of aerosol, ozone, and solar ultraviolet irradiance in the troposphere

Modeling of ozone reactions on aircraft-related soot in the upper troposphere and lower stratosphere

Column-integrated aerosol optical properties in the free troposphere: case study-Sierra Nevada, Spain

Florida thunderstorms: A faucet of reactive nitrogen to the upper troposphere

Distributing characters of physical factors on two types of easterly air steam in lower troposphere

Troposphere Delay Calculation with Multi-parameter Estimates

Impact of monsoon circulations on the upper troposphere and lower stratosphere

Photodissociation of acetone in the troposphere: an algorithm for the quantum yield

Turbulence parameters in the tropical troposphere and lower stratosphere

Global distribution and sources of volatile and nonvolatile aerosol in the remote troposphere

Late-spring increase of trans-Pacific pollution transport in the upper troposphere

Concentrations and sources of organic carbon aerosols in the free troposphere over North America

Discussion on the height of Meteorological Measurement in high troposphere

Analysis of the Troposphere Level Delay for Precision Positioning in GPS

Analysis on Tropical and Subtropical Vapour Field in Upper- middle Troposphere

Characteristics of Water Vapour Transfer in Upper - middle Troposphere over Xinjiang

The Application of Chirp in Troposphere Scatter Communication

Remote Sensing Water Vapor Content in Atmospheric Troposphere with GPS

Lidar Measurements of Cloud and Aerosol in the Upper Troposphere in Beijing

Advances and Prospects in the Study of Stratosphere-Troposphere Exchange

Origin of Lapse Rate Changes in the Upper Tropical Troposphere

Evidence of the solar cycle in the tropical troposphere

Role of convection in global-scale transport in the troposphere

Courses of the troposphere heating

Dynamic feedbacks of troposphere aerosols on marine low cloud during boreal spring

Dynamic feedbacks of troposphere aerosols on marine low cloud during boreal spring

Intraseasonal variations of water vapor and cirrus clouds in the tropical upper troposphere

The Influence of Increasing Ozone in Troposphere on Air Temperature in China