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The equatorial and low-latitude ionosphere within the context of global modeling

The equatorial and low-latitude ionosphere within the context of global modeling
The equatorial and low-latitude ionosphere within the context of global modeling
The thermosphere–ionosphere–mesosphere-electrodynamics coupled model TIME-GCM, coupled to NCEP lower atmosphere data, is used to simulate the noontime ionospheric peak electron density NmF2 at low latitudes for year 2002. Model output are compared with observations a three ionosonde stations: Jicamarca, Ascension Island and Darwin, stations at geomagnetic latitudes of 3°S, 10°S and 22°S, respectively. The modeled electron density at the peak of the F2-layer (NmF2) matches the general trend of the data fairly well at noon throughout the year. The shapes of the diurnal curves of NmF2 vs. local time are not well produced in the model, and particularly so at the two stations away from the geomagnetic equator. At all sites the day-to-day variability of NmF2, assessed using the percent standard deviation about the monthly mean, is about twice the modeled variability. Possible sources of this shortfall in the model may be due to the under-representation of coupling from below and/or from auroral sources
ionospheric variability, general circulation modeling, coupling of atmospheric regions, equatorial aeronomy, low-latitude ionosphere
1364-6826
358-368
Mendillo, Michael
4eddc349-753b-4f7f-96c7-b1b6c7715fa0
Wroten, Joei
c40fcef2-29bb-4bf9-acb7-70aba63ecd57
Roble, Raymond
21d639bd-5ad9-4a1a-bc26-5ca210e12021
Rishbeth, Henry
472ad744-0f44-4325-9930-c2c06cdbf4a3
Mendillo, Michael
4eddc349-753b-4f7f-96c7-b1b6c7715fa0
Wroten, Joei
c40fcef2-29bb-4bf9-acb7-70aba63ecd57
Roble, Raymond
21d639bd-5ad9-4a1a-bc26-5ca210e12021
Rishbeth, Henry
472ad744-0f44-4325-9930-c2c06cdbf4a3

Mendillo, Michael, Wroten, Joei, Roble, Raymond and Rishbeth, Henry (2010) The equatorial and low-latitude ionosphere within the context of global modeling. Journal of Atmospheric and Solar-Terrestrial Physics, 72 (4), 358-368. (doi:10.1016/j.jastp.2009.03.026).

Record type: Article

Abstract

The thermosphere–ionosphere–mesosphere-electrodynamics coupled model TIME-GCM, coupled to NCEP lower atmosphere data, is used to simulate the noontime ionospheric peak electron density NmF2 at low latitudes for year 2002. Model output are compared with observations a three ionosonde stations: Jicamarca, Ascension Island and Darwin, stations at geomagnetic latitudes of 3°S, 10°S and 22°S, respectively. The modeled electron density at the peak of the F2-layer (NmF2) matches the general trend of the data fairly well at noon throughout the year. The shapes of the diurnal curves of NmF2 vs. local time are not well produced in the model, and particularly so at the two stations away from the geomagnetic equator. At all sites the day-to-day variability of NmF2, assessed using the percent standard deviation about the monthly mean, is about twice the modeled variability. Possible sources of this shortfall in the model may be due to the under-representation of coupling from below and/or from auroral sources

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More information

Published date: March 2010
Keywords: ionospheric variability, general circulation modeling, coupling of atmospheric regions, equatorial aeronomy, low-latitude ionosphere

Identifiers

Local EPrints ID: 148111
URI: http://eprints.soton.ac.uk/id/eprint/148111
ISSN: 1364-6826
PURE UUID: 41a0a698-ec5c-4e81-9720-c0522598b0ea

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Date deposited: 27 Apr 2010 10:55
Last modified: 14 Mar 2024 01:01

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Contributors

Author: Michael Mendillo
Author: Joei Wroten
Author: Raymond Roble
Author: Henry Rishbeth

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