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Spatial and temporal variation in lightning ignitions in Sweden
Author(s) -
Granström Anders
Publication year - 1993
Publication title -
journal of vegetation science
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.1
H-Index - 115
eISSN - 1654-1103
pISSN - 1100-9233
DOI - 10.2307/3235609
Subject(s) - lightning (connector) , precipitation , physical geography , spatial distribution , atmospheric sciences , geography , environmental science , lightning strike , meteorology , geology , thunderstorm , remote sensing , physics , power (physics) , quantum mechanics
. Analysis of fire statistics revealed that there are steep gradients in the distribution of lightning‐caused fire ignitions in Sweden. The highest ignition density was found in the southeastern provinces of Kalmar and Östergötland, ca. 0.23/10 000 ha/yr. From there, densities generally declined both to the north and to the west, with a density averaging ca. 0.05 in the six northernmost provinces, and an equally low density in the southwestern province of Halland. For both northern and southern Sweden, lightning ignitions peaked in early July, but in the south the season for ignitions started 2–3 weeks earlier and ended 2–3 weeks later. The geographical gradients in lightning ignition density correspond to the average precipitation during summer. The patterns of lightning ignition densities may also indicate gradients in natural fire frequencies. This hypothesis is supported by the distribution of certain fire‐adapted plant species.