North Core Banks, North Carolina before Hurricane Dorian (2019) breached the barrier island from the backbarrier side (outwash), immediately after, and recovery over the following three years.
Coastal morphodynamics and coastal change
Nearly 40% of the global population lives in coastal communities, subject to increasing climate hazards. We seek to understand and improve models of fundamental coastal processes that introduce hazards to communities during extreme events. The coastal ocean is a dynamic environment dominated by wave breaking, wave-driven currents, and larger-scale tidal and wind-driven circulation. These nearshore processes drive rapid evolution of nearshore bathymetry, such as migration of bars or inlet deltas, and subaerial topography, such as erosion, breaching, or recovery of beaches, barrier complexes, and bluffs.
We are investigating questions including:
Select relevant publications
M. Olabarrieta, J.C. Warner, and C.A. Hegermiller, 2023. Development and application of an Infragravity Wave (InWave) driver to simulate nearshore processes. Journal of Advances in Modeling Earth Systems. doi:10.1029/2022MS003205
Hegermiller, C.A., J.C. Warner, M. Olabarrieta, C.R. Sherwood, and T.S. Kalra, 2022. Barrier island breach dynamics during Hurricanes Sandy and Matthew. Journal of Geophysical Research: Earth Surface. doi.org/10.1029/2021JF006307
Sherwood, C.R., A. Van Dongeren, J. Doyle, C.A. Hegermiller, and others, 2021. Modeling the morphodynamics of coastal responses to extreme events: What shape are we in? Annual Review of Marine Sciences. doi: 10.1146/annurev-marine-032221-090215
West Cliff, Santa Cruz, CA withstanding tremendous wave energy during an early El Nino storm in January 2016.
Ocean wave dynamics, climate, and forecasting
The coastal ocean is subject to remote or non-local forcings, most notably waves propagating into the nearshore from distant generation regions. To improve predictions of coastal dynamics, it is thus necessary to expand understanding and improve forecasting of ocean wave dynamics. Further, characterizing historical and potential future ocean wave climate is critical to predict changes to coastal wave energy and coastal response over long time scales, such as the next century.
We are investigating questions including:
Select relevant publications
Hegermiller, C.A., J.C. Warner, M. Olabarrieta, and C.R. Sherwood, 2019. Wave-current interaction between Hurricane Matthew wave fields and the Gulf Stream. Journal of Physical Oceanography. doi: 10.1175/JPO-D-19-0124.1
Houghton, I. A., C.A. Hegermiller, C. Teicheira, and P.B. Smit, 2022. Operational assimilation of spectral wave data from the Sofar Spotter network. Geophysical Research Letters, 49, e2022GL098973. https://doi. org/10.1029/2022GL098973
Hegermiller, C.A., A. Rueda, L.H. Erikson, P.L. Barnard, J.A.A. Antolinez, and F.J. Mendez, 2017. Controls of multimodal wave conditions in a complex coastal setting. Geophysical Research Letters, 44, doi: 10.1002/2017GL075272
Hegermiller, C.A., J.A.A. Antolinez, A. Rueda, P. Camus, J. Perez, L.H. Erikson, P.L. Barnard, and F.J. Mendez, 2016. A wave spectrum-based approach to defining the predictor for statistical downscaling of local wave climate. Journal of Physical Oceanography, 47, doi: 10.1175/JPO-D-16-0191.1