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Boundary layer ozone and cloud coverage at Paramaribo Station (5.8N 55.2W)
This report covers the first results of two new parameters measured at the para-maribo station af...
Stijn Maas | Year: 2004 | Pages: 40
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Voortplanting van zwaartegolven in de atmosfeer en rond een kritieke laag
The atmosphere is a continuous, layered medium with vertical gradients in density caused by gravi...
E.R. Stolp | Year: 1985 | Pages: 80
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Grass pollen counts in the West Netherlands as a function of the weather conditions
Eight hundred and ten four-hourly mean grass pollen counts (observed in Leiden, west-Netherland) ...
J.F. den Tonkelaar | Year: 1986 | Pages: 157
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An indirect estimate of the predictability of the monthly mean atmosphere
It is sometimes claimed that the near-constant anomalies in external conditions produce an atmosp...
H.M. van den Dool | Year: 1981 | Pages: 28
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Microgravity as a tool for eruption forecasting
Detection of gravity change over time has been used to better understand magmatic activity at vol...
Elske de Zeeuw - van Dalfsen,
Michael P. Poland | Journal: Journal of Volcanology and geothermal research | Volume: 442 | Year: 2023 | doi: https://doi.org/10.1016/j.jvolgeores.2023.107910
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