nounthe lowest atmospheric layer Related Words layer atmosphere tropopause Based on WordNet 3.0, Farlex clipart collection. © 2003-2012 Princeton University, Farlex Inc. Want to thank TFD for its existence?Tell a friend about us, add a link to this page, or visitthe webmaster's page for...
(Physical Geography) the lowest atmospheric layer, about 18 kilometres (11 miles) thick at the equator to about 6 km (4 miles) at the Poles, in which air temperature decreases normally with height at about 6.5°C per km troposphericadj ...
in particular related to terrorism, posed by the proliferation of all arms and related materiel of all types, in particular man-portable surface-to-air missiles, from Libya in the region, and to submit a report to the Council on proposals to counter th[at] threat, and to prevent the proli...
Such radars, as well as providing additional information about the clear-air patterns observed previously, enable continuous measurements of wind profiles to be made. This paper describes the phenomena which have been observed and the measurements which have been made with radars under clear-air ...
The detailed structure of upper-air temperature trends is more demanding to determine. For decades, observations of upper-air temperature trends have either been of poor vertical resolution, or of limited horizontal coverage. In the first case, the layer-averaged measurements from the Microwave ...
What is the air pressure in the troposphere? What is responsible for the weather patterns in the troposphere? What are atmospheric conditions like in the troposphere and stratosphere? What is the difference between the troposphere and the thermosphere?
Abstract First free tropospheric (0–8 km) peroxyacetyl nitrate (CH3C(O)OONO2, PAN) measurements in the clean marine air of the Pacific (36–40 °N) show that the tropospheric reservoir of nitrogen oxides (NO, NO2) may be 30–50% larger than hitherto believed. We show here that these...
(210Pb) activity concentration in surface layer air (SL) about 1.5 m height above ground level were performed on Raciborz meteorological station (geographical coordinates: latitude 50°03'42" N, longitude 18°11'30" E, 206 m height above sea level), that belongs to The National Weather ...
information of the amount of zenith troposphere delay to be used by a user located in point A (user point) are set up, an estimated value ZTDB of said amount of zenith troposphere delay in this reference point B is calculated, the information about the correction value of the amount of ...
A study of the fine structure of air refractivity in the lower troposphere has been continued through the spring and summer of 1962 by the observation of weak radio reflections from clear air (radar angels), with a vertically directed radar of special design operating at 6770 Mc/s. These ...