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Journal ArticleDOI

MPM—An atmospheric millimeter-wave propagation model

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TLDR
In this paper, the authors characterized the neutral atmosphere for the frequency range from 1 to 300 GHz as a nonturbulent propagation medium and predicted attenuation and propagation delay effects from meteorological data sets: pressure, temperature, humidity, suspended particle concentration, and rain rate.
Abstract
The neutral atmosphere is characterized for the frequency range from 1 to 300 GHz as a nonturbulent propagation medium. Attenuation and propagation delay effects are predicted from meteorological data sets: pressure, temperature, humidity, suspended particle concentration, and rain rate. The physical data base of the propagation model consists of four terms: (a) resonance information for 30 water vapor and 48 oxygen absorption lines in the form of intensity coefficients and center frequency for each line; (b) a composite (oxygen, water vapor, and nitrogen) continuum spectrum; (c) a hydrosol attenuation term for haze, fog, ,and cloud conditions; and (d) a rain attenuation model. Oxygen lines extend into the mesosphere, where they behave in a complicated manner due to the Zeeman effect. The geomagnetic field strength H is required as an additional input parameter. Each 02 line splits proportionally with H into numerous, sub-lines, which are juxtaposed to form a Zeeman pattern spread over a megahertz scale. Patterns for three main polarization cases are calculated. Detailed examples for model atmospheres provide basic millimeter wave propagation information over the height range 0 to 100 km of the neutral atmosphere.

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Citations
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Proceedings ArticleDOI

Atmospheric gas impact on fixed satellite communication link a study of its effects at Ku, Ka and V bands in Nigeria

TL;DR: In this article, the total atmospheric absorption due to Oxygen and water vapour on the earth-space path at Ku (12/14 GHz), Ka (20/30 GHz), and V (40/50 GHz) bands was evaluated for communication with Nigeria communication satellite (Nigcomsat1) on both uplink and down link at 0.01 % unavailability of an average year.
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Remote sensing of boundary-layer temperature profiles by a scanning 5-mm microwave radiometer and RASS: a comparison experiment

TL;DR: In this paper, two techniques for deriving low-altitude temperature profiles were evaluated at an experiment conducted from November 1996 to January 1997 at the Boulder Atmospheric Observatory (BAO).
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Observation of a strong inverse temperature dependence for the opacity of atmospheric water vapor in the mm continuum near 280 GHz

TL;DR: In this article, the authors used atmospheric opacity measurements made at 278 GHz (9.3 cm−1) at McMurdo Station, Antarctica during the austral springs of 1986 and 1987, combined with measurements of water vapor profile and total column density from near-simultaneous balloon flights, to determine the attenuation per mm of precipitable water vapor (pwv) at this frequency.
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Performance of Radiative Transfer Models in the Microwave Region

TL;DR: In this article, the authors compared two fast radiative transfer models, Community Radiative Transfer Model (CRTM) and Radious Transfer for TIROS Operational Vertical Sounder (RTTOV), with the LBL model Atmospheric Radiative Transfer Simulator (ARTS).

Validation of Satellite-Derived Liquid Water Paths Using ARM SGP Microwave Radiometers

TL;DR: In this paper, the authors compared the relationship between the GOES-8 and microwave LWP retrievals as related to cloud temperature, cloud type, and viewing angle, using data taken in a variety of cloud conditions during March 2000.
References
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Journal ArticleDOI

The aR b relation in the calculation of rain attenuation

TL;DR: In this paper, the empirical relation A = aR^{b} between the specific attenuation A and the rain rate R is used in the calculation of rain attenuation statistics.
Journal ArticleDOI

An updated model for millimeter wave propagation in moist air

Hans J. Liebe
- 01 Sep 1985 - 
TL;DR: In this article, a practical atmospheric millimeter-wave propagation model (MPM) is proposed to predict attenuation for dry air at 2.5-430 GHz. But the model is limited to frequencies below 300 GHz and the number of spectroscopic parameters can be reduced to less than 200.
Journal ArticleDOI

Electromagnetic wave propagation and scattering in rain and other hydrometeors

T. Oguchi
TL;DR: In this paper, the authors review the theories and results of numerical calculations of interactions between hydrometeors and microwaves or millimeter waves propagating in media containing these hydrometers.
Journal ArticleDOI

Millimeter-wave attenuation and delay rates due to fog/cloud conditions

TL;DR: In this paper, the propagation properties of suspended water and ice particles which make up atmospheric haze, fog, and clouds were examined for microwave and millimeter-wave frequencies, and the rates of attenuation alpha (dB/km) and delay tau (ps/km), derived from a complex refractivity based on the Rayleigh absorption approximation of Mie's scattering theory, were derived.
Journal ArticleDOI

Interference coefficients for overlapping oxygen lines in air

TL;DR: In this article, the interference coefficients were determined for the 5-mm wavelength oxygen lines broadened by air and solved by the Twomey-Tikhonov method, which minimizes a cost function, subject to the condition of constant measurement error variance.
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