Noun:

ट्रोपोस्फियर,

tropospheric's Usage Examples:

describe two distinct phenomena; the stratospheric polar vortex, and the tropospheric polar vortex.

An upper tropospheric cyclonic vortex is a vortex, or a circulation with a definable center, that usually moves slowly from east-northeast to west-southwest.

with no changes in stratospheric dynamics, no surface and tropospheric feedbacks in operation (i.

mechanisms, such as tropospheric scattering (troposcatter), tropospheric ducting (ducting), and near vertical incidence skywave (NVIS) which are used in specialized.

the formation of smog and acid rain, as well as affecting tropospheric ozone.

MOZART was designed to simulate tropospheric chemical and transport processes, but has been extended into the stratosphere.

Mid-tropospheric systems, such as the subtropical ridge, deflect tropical cyclones around.

by plants to carry out photosynthesis and leads to the production of tropospheric ozone which damages plants.

|-|3D-Winds|stylebackground:#eee;|Proposed|NASA||Monitor tropospheric winds for weather forecasting and pollution transport.

Surface-based Upper level Cold-core low Polar vortex Upper tropospheric cyclonic vortex.

cases, convection-induced winds take on a bow echo (backward "C") form of squall line, often forming beneath an area of diverging upper tropospheric winds.

Upper level cyclones can exist without the presence of a surface low, and can pinch off from the base of the tropical upper tropospheric.

A tropical upper tropospheric trough (TUTT), also known as the mid-oceanic trough, is a trough situated in upper-level (at about 200 hPa) tropics.