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 ...
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| Dokumenttyp: | Dataset |
| Erscheinungsdatum: | 2022 |
| Verlag/Hrsg.: |
PANGAEA
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| Schlagwörter: | DATE/TIME / Air electric potential gradient / uncertainty / Air temperature at 2 m height / Humidity / relative / Precipitation / Short-wave downward GLOBAL radiation / Wind speed / standard deviation / Wind direction / Pressure / atmospheric / Snow coverage / Snow thickness / Cloud cover / low clouds / Cloud base height / Climate monitoring station / Geophysical Observatory Reports / Calculated / Campbell meteorological station / ERA5-Land hourly data 1950 to present dataset Muñoz Sabater / 2019 / 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 |
| Sprache: | Englisch |
| Permalink: | https://search.fid-benelux.de/Record/base-29265376 |
| Datenquelle: | BASE; Originalkatalog |
| Powered By: | BASE |
| Link(s) : | https://dx.doi.org/10.1594/pangaea.942036 |
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 traditionally referred to as “fair weather” and is characterized by allowed ranges of specified meteorological parameters. This is why information on the actual weather condition is supposed to be an inherent supplement of PG datasets.This dataset contains PG data recorded in the Széchenyi István Geophysical Observatory (NCK, 47.632°N, 16.718°E), Hungary from 1962, when the regular measurements were started, up to 2009. ...