Please use this identifier to cite or link to this item: http://library.iigm.res.in:8080/xmlui/handle/123456798/294
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dc.contributor.authorJadhav, Ashish
dc.contributor.authorSubramanian, Gurubaran
dc.contributor.authorPatil, Parashram
dc.date.accessioned2022-08-04T06:14:26Z
dc.date.available2022-08-04T06:14:26Z
dc.date.issued2022
dc.identifier.citationEGU22-9390, EGU General Assembly 2022, https://doi.org/10.5194/egusphere-egu22-9390en_US
dc.identifier.urihttp://library.iigm.res.in:8080/xmlui/handle/123456798/294
dc.description.abstractThe coupled response of the atmosphere-ionosphere system to planetary waves propagating from below has been observed through MF and Meteor radars at different longitudes along with the ground geomagnetic data from 23 stations of Northern (NH) and Southern Hemisphere (SH) during northern winter months of January, 2015 and 2017. The focus is on delineating the quasi-2-day (Q2DW) and quasi-6-day wave signatures in the mesosphere-lower thermosphere (MLT) and in ionospheric Sq currents besides deciphering their effects on the overall neutral dynamics at low latitudes. Analysis extended to longitudinally separated stations confirms the penetration of these planetary waves into the ionosphere either directly or indirectly through interaction with other wave modes in the MLT region.en_US
dc.language.isoenen_US
dc.subjectPlanetary waveen_US
dc.subjectAtmosphereen_US
dc.titlePlanetary wave activity observed in atmosphere-ionosphere system over low latitudesen_US
dc.typeArticleen_US
dcterms.sourcehttps://doi.org/10.5194/egusphere-egu22-9390
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