Atmospheric electric potential gradient data and measured as well as reanalyzed meteorological parameters at the Széchenyi István Geophysical Observatory, Hungary, from the years 1962-2009

The negative of the vertical component of the atmospheric direct current (DC) electric field is referred to as the atmospheric electric potential gradient (PG). The PG depends on the actual ionospheric potential, local electric fields, and the electrical conductivity of the air at the place of the measurement. These factors are more or less directly connected to meteorological conditions. The overall state of the global network of large-scale electrical currents in the Earth-ionosphere system can be inferred from the PG when the weather is locally calm. This meteorological condition is traditi... Mehr ...

Volltext
Verfasser: Buzás, Attila
Szabóné André, Karolina
Bór, József
Dokumenttyp: Dataset
Erscheinungsdatum: 2022
Verlag/Hrsg.: PANGAEA
Schlagwörter: 1962-1978: ERA5 hourly data on single levels 1950-1978 (preliminary version) dataset (Bell et al. / 2020) / 1979-2009: derived from the ERA5 hourly data on single levels 1979 to present dataset (Herschbach et al. / 2018) / Air electric potential gradient / uncertainty / Air temperature at 2 m height / Calculated / Campbell meteorological station / Climate monitoring station / Cloud base height / Cloud cover / low clouds / CMS / DATE/TIME / ERA5-Land hourly data 1950 to present dataset (Muñoz Sabater / 2019) / Geophysical Observatory Reports / Humidity / relative / Hungary / Nagycenk / NCK / Precipitation / Pressure / atmospheric / Short-wave downward (GLOBAL) radiation / Snow coverage / Snow thickness / Wind direction / standard deviation / Wind speed
Sprache: Englisch
Permalink: https://search.fid-benelux.de/Record/base-26869492
Datenquelle: BASE; Originalkatalog
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Link(s) : https://doi.pangaea.de/10.1594/PANGAEA.942036