By J. Bret Bennington, E. Christa Farmer
Learning from the affects of Superstorm Sandy summarizes first effects from reports of Superstorm Sandy, together with: tide gauge measurements of hurricane surge, seashore survey and lidar measurements of geomorphological alterations, sturdy isotope version in precipitation, research of the impression of seashore nourishment between different components on structural harm, and comparability with earlier storms via sediment research. This e-book offers a multi-dimensional therapy of clinical result of reports of Superstorm Sandy, and it's a worthwhile reference for oceanographers, coastal geologists, climatologists, dynamic meteorologists, paleotempostologists, sedimentary geologists, geomorphologists and emergency managers who have to higher comprehend the hurricane and its results that allows you to be ready for comparable occasions sooner or later.
- Summarizes first effects from reviews of Superstorm Sandy
- Gives a multi-dimensional therapy of clinical result of stories of Superstorm Sandy
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Additional info for Learning from the impacts of superstorm sandy
4). 7) are located in the south and west of the study domain. These represent the downwind regions of the storm circulation, where air masses had longer over-land fetch. These isotope data suggest that rainout rates far exceeded the resupply of moisture from the land surface along these circulation trajectories, and by the time air parcels have reached the southwest quadrant of the storm much of their vapor had precipitated out. The highest rainout fractions were observed shortly after landfall, consistent with the peak in rain rates at coastal mid-Atlantic sites.
2002. Stable isotope ratios: Hurricane L Olivia. Journal of Atmospheric Chemistry 41 (1), 67–82. , 1998. Stable isotope ratios of rain and vapor L in 1995 hurricanes. Journal of Geophysical Research Atmospheres 103 (D10), 11381–11400. , 1996. Low stable isotope ratios of tropical cyclone rains. L Geophysical Research Letters 23 (5), 527–530. , 2013. Lagrangian Modeling of the Atmosphere, chapter Lagrangian Modeling of the L Atmosphere, An Introduction. American Geophysical Union, AGU Geophysical Monograph.
0‰. 1‰), and then slowly began to rise. The trend in deuterium excess at the Colcord site is indicative of a mix of precipitation from the midlatitude trough and Sandy associated waters. 5‰. 4‰ and remained steady at these levels. 3 LAGRANGIAN BACK-TRAJECTORY ANALYSIS In order to assess the isotopic evolution of cyclonic moisture associated with Superstorm Sandy, information is needed on the isotopic composition of source moisture (d0). , 2014). Here we use the stochastic time-inverted Lagrangian transfer (STILT) model to estimate the source vapor isotopic composition for each hour that precipitation was collected at the four focus sites.