Extreme point rainfal temporal scaling and associated atmospheric processes
Resumen
The study describes an analysis of point rainfall amounts obtained from raingauge measurements in Spain covering periods from 10 minutes to 2 years, their temporal scaling and a discussion of predominant atmospheric processes involved. A large database exceeding 11,000 stations, some of which with more than 200 years records, was used and results are compared against corresponding world rainfall records.Citas
Craig, G. C., T. Selz, T, 2018: Mesoscale Dynamical Regimes in the Midlatitudes. Geophys. Res. Let., 45, 410-417.
Fujita, T. T., 1981: Tornadoes and downbursts in the context of generalized planetary scales. J. Atmos. Sci., 38, 1511-1534.
Galmarini, S., D. G. Steyn, B. Ainslie, 2004: The scaling law relating world point‐precipitation records to duration. Int. J. Climatol., 24, 533-546.
Gonzalez, S., J. Bech, 2017: Extreme point rainfall temporal scaling: a long term (1805–2014) regional and seasonal analysis in Spain. Int. J. Climatol., 37, 5068-5079.
Jennings, A.H., 1950: World’s greatest observed point rainfalls. Mon. Wea.Rev., 78, 4-5.
Monjo, R., J. Martin-Vide, 2016: Daily precipitation concentration around the world according to several indices. Int. J. Climatol. 36, 3828–3838.
