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- > Magnitude and frequency in geomorphology (supprimer)
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Par Collection Par Auteur- CROZIER, M., (Editeur scientifique) (3)
- FAVIS-MORTLOCK, D. (1)
- FRAGOSO, M. (1)
- BOARDMAN, J. (1)
- BRANDÃO, C. (1)
- PRESTON, N.J. (1)
- 1999 (3)
- Agroclimatologie ; Climatologie synoptique ; Domaine aride ; Domaine méditerranéen ; Erosion pluviale ; Evora ; Orage ; Portugal ; Précipitation ; Régime pluviométrique ; Variabilité interannuelle ; Variation spatiale (1)
- Agroclimatology ; Arid area ; Evora ; Interannual variability ; Mediterranean area ; Portugal ; Precipitation ; Raindrop erosion ; Rainfall regime ; Rainstorm ; Spatial variation ; Synoptic climatology (1)
- Altérite ; Bassin-versant ; Classification ; Erosion des sols ; Glissement de terrain ; Modélisation ; North Island ; Nouvelle-Zélande ; Propriétés du sol ; Précipitation ; Prévision ; Risque naturel (1)
- Belgique ; Bilan d'érosion ; Canada ; Concept ; Erosion des sols ; Etats-Unis ; Fréquence et magnitude ; Précipitation ; Royaume-Uni ; Ruissellement ; Régression linéaire ; Versant (1)
- Belgium ; Canada ; Concept ; Erosion budget ; Linear regression ; Precipitation ; Rill wash ; Slope ; Soil erosion ; United Kingdom ; United States of America (1)
- Magnitude and frequency in geomorphology (3)
- Event-induced changes in landsurface condition - implications for subsequent slope stability (1)
- Extreme storms and rainfall erosivity factor in Évora (Portugal) (1)
- Frequency-magnitude distributions for soil erosion, runoff and rainfall - a comparative analysis (1)
- Frequency-magnitude distributions for soil erosion, runoff and rainfall - a comparative analysis
- This study analyses frequency-magnitude distributions of rainfall, runoff and erosion from sites in the UK, Belgium, Canada and the USA. Frequency-magnitude distributions of rainfall appear to be a poor predictor of distributions of runoff or soil
- Extreme storms and rainfall erosivity factor in Évora (Portugal)
- Agroclimatology ; Arid area ; Evora ; Interannual variability ; Mediterranean area ; Portugal ; Precipitation ; Raindrop erosion ; Rainfall regime ; Rainstorm ; Spatial variation ; Synoptic climatology
- to change. It is concluded that the relation of erosional response to rainfall input is not stable over time and that thresholds are unstable.