More Like this

1. The dynamics of intensification in a Hurricane Weather Research and Forecasting simulation of Hurricane Earl (2010): HWRF Simulation of Hurricane Earl (2010)

   https://doi.org/10.1002/qj.2922  

   Smith, Roger K. ; Zhang, Jun A. ; Montgomery, Michael T. ( January 2017 , Quarterly Journal of the Royal Meteorological Society)
2. Contrasting Hurricane Ike washover sedimentation and Hurricane Harvey flood sedimentation in a Southeastern Texas coastal marsh

   https://doi.org/10.1016/j.margeo.2019.106011  

   Williams, Harry ; Liu, Kam-biu ( November 2019 , Marine Geology)
3. Hurricane Deposits on Carbonate Platforms: a case study of Hurricane Irma deposits on Little Ambergris Cay, Turks and Caicos Islands

   https://doi.org/10.1029/2020JF005597  

   Jamison‐Todd, Sarah ; Stein, Nathan ; Overeem, Irina ; Khalid, Arslaan ; Trower, Elizabeth J. ( June 2020 , Journal of Geophysical Research: Earth Surface)

   The study of modern hurricane deposits is useful both in identifying ancient hurricane deposits in the rock record and predicting patterns of deposition and erosion produced by future storm events. Hurricane deposits on carbonate platforms have been studied less frequently than those along continental coasts. Here we present observations of the characteristics of deposition and scour caused by Hurricane Irma on Little Ambergris Cay, a small uninhabited island located near the southeastern edge of the Caicos platform in the Turks and Caicos Islands. Hurricane Irma passed directly over Little Ambergris Cay on September 7, 2017 as a Category 5 hurricane. We described and sampled multiple types of hurricane deposits and determined that the washover fans were the best sedimentological records for hurricane conditions, as they were subject to very little reworking over time. We compared different model predictions of storm tide and wave height with eyewitness reports and distributions of scour. Examining the washover fans allowed for the construction of a conceptual model for hurricane deposits formed in a high‐energy storm event on a carbonate platform. Characteristics of the washover fans were their small size, the lack of sedimentary structures, and very well‐sorted sediment. The size and distribution of carbonatemore »boulders eroded and transported by the storm are consistent with depth‐averaged flow velocities in the range of 1.5‐5.3 m/s. The strength of the storm and the low‐lying topography, distinct features of a carbonate platform setting, contributed to high levels of sediment bypass and high flow velocities, resulting in small, unstructured deposits.« less
4. Transition of the Hurricane Boundary Layer during the Landfall of Hurricane Irene (2011)

   https://doi.org/10.1175/JAS-D-19-0290.1  

   Alford, A. Addison ; Zhang, Jun A. ; Biggerstaff, Michael I. ; Dodge, Peter ; Marks, Frank D. ; Bodine, David J. ( October 2020 , Journal of the Atmospheric Sciences)

   Abstract The hurricane boundary layer (HBL) has been observed in great detail through aircraft investigations of tropical cyclones over the open ocean, but the coastal transition of the HBL has been less frequently observed. During the landfall of Hurricane Irene (2011), research and operational aircraft over water sampled the open-ocean HBL simultaneously with ground-based research and operational Doppler radars onshore. The location of the radars afforded 13 h of dual-Doppler analysis over the coastal region. Thus, the HBL from the coastal waterways, through the coastal transition, and onshore was observed in great detail for the first time. Three regimes of HBL structure were found. The outer bands were characterized by temporal perturbations of the HBL structure with attendant low-level wind maxima in the vicinity of rainbands. The inner core, in contrast, did not produce such perturbations, but did see a reduction of the height of the maximum wind and a more jet-like HBL wind profile. In the eyewall, a tangential wind maximum was observed within the HBL over water as in past studies and above the HBL onshore. However, the transition of the tangential wind maximum through the coastal transition showed that the maximum continued to reside in the HBLmore »through 5 km inland, which has not been observed previously. It is shown that the adjustment of the HBL to the coastal surface roughness discontinuity does not immediately mix out the residual high-momentum jet aloft. Thus, communities closest to the coast are likely to experience the strongest winds onshore prior to the complete adjustment of the HBL.« less
5. Hurricane-induced power outage risk under climate change is primarily driven by the uncertainty in projections of future hurricane frequency,

   https://doi.org/doi.org/10.1038/s41598-020-72207-z  

   N. Alemazkoor, B. Rachunok ( January 2020 , Scientific reports)