Optimising rainfall characteristics for determining landslide thresholds. [PDF]
Abeysiriwardana H, Kjeldsen T, Reale C.
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Fading Attention and the Pricing of Default Risk in the German Market for Structured Products
ABSTRACT Structured retail products are unsecured bonds subject to the default risk of the issuer. We analyze the price‐setting policy of issuers with respect to this default risk. Using a long‐term data set of discount certificates in the German market, we apply a time series IVX‐approach to find that (i) quoted prices do depend on issuer default risk,
Rainer Baule, Falk Jensen
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Climate Variability Drives Dengue Transmission in Bangladesh. [PDF]
Siddiqa A +5 more
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This work advances landslide susceptibility mapping by incorporating short‐term trigger data with landscape susceptibility mapping. We also examine the importance of downsampling, watershed delineation and geospatial correlations in evaluating outcomes.
Kanta Kotsugi +3 more
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Assessment of landslide hazard under specific rainfall scenarios based on a hybrid CNN-TRIGRS and matrix approach: a case study of Meishan Town, Zhejiang Province, China. [PDF]
Wang Z +5 more
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Archeological data with AI- and physics-based modeling explain typhoon-induced disasters in inland China around 3000 yr B.P. [PDF]
Ding K +18 more
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Evaluating the RUNOFF01 model's performance and potential for micro-catchment design. [PDF]
Shabani A, Roodari A, Sepaskhah AR.
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Mega-floods over the past 30,000 years in western yunnan, southwest China. [PDF]
Suo Q +7 more
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Rainfall Intensities for Southeastern Arizona
Journal of Irrigation and Drainage Engineering, 1988Small watershed storm runoff in the southwestern United States is dominated by intense, short-duration convective rains of limited areal extent. Most commonly, flood peak estimates are based on rainfall predictions found in the National Oceanic and Atmospheric Administration (NOAA) Atlas 2, a precipitation-frequency atlas for the Western United States.
Herbert B. Osborn, Kenneth G. Renard
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Statistics of the total time, in minutes, that extreme rainfall rates are exceeded were computed from weighing raingage records at stations in several rainfall regimes. The results are presented on maps, frequency diagrams and as analytical expressions. Measures of areal variability were calculated from data at seven stations within an 8 km2 area.
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