Item talk:Q306065
From geokb
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"name": "Hillslopes in humid-tropical climates aren\u2019t always wet: Implications for hydrologic response and landslide initiation in Puerto Rico, USA",
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"abstract": "The devastating impacts of the widespread flooding and landsliding in Puerto Rico following the September 2017 landfall of Hurricane Maria highlight the increasingly extreme atmospheric disturbances and enhanced hazard potential in mountainous humid\u2010tropical climate zones. Long\u2010standing conceptual models for hydrologically driven hazards in Puerto Rico posit that hillslope soils remain wet throughout the year, and therefore, that antecedent soil wetness imposes a negligible effect on hazard potential. Our post\u2010Maria in situ hillslope hydrologic observations, however, indicate that while some slopes remain wet throughout the year, others exhibit appreciable seasonal and intra\u2010storm subsurface drainage. Therefore, we evaluated the performance of hydro\u2010meteorological (soil wetness and rainfall) versus intensity\u2010duration (rainfall only) hillslope hydrologic response thresholds that identify the onset of positive pore\u2010water pressure, a predisposing factor for widespread slope instability in this region. Our analyses also consider the role of soil\u2010water storage and infiltration rates on runoff generation, which are relevant factors for flooding hazards. We found that the hydro\u2010meteorological thresholds outperformed intensity\u2010duration thresholds for a seasonally wet, coarse\u2010grained soil, although they did not outperform intensity\u2010duration thresholds for a perennially wet, fine\u2010grained soil. These end\u2010member soils types may also produce radically different stormflow responses, with subsurface flow being more common for the coarse\u2010grained soils underlain by intrusive rocks versus infiltration excess and/or saturation excess for the fine\u2010grained soils underlain by volcaniclastic rocks. We conclude that variability in soil\u2010hydraulic properties, as opposed to climate zone, is the dominant factor that controls runoff generation mechanisms and modulates the relative importance of antecedent soil wetness for our hillslope hydrologic response thresholds.",
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