This project overview describes a 2017-18 science transfer project led by the Narragansett Bay National Estuarine Research Reserve that developed a regional workshop to build capacity for New England salt marsh resilience.

This project overview describes a 2018 Catalyst project where Rookery Bay Reserve staff and University of South Florida researchers are partnered to update and create maps of mangrove habitat to measure changes over time.

This summary brochure describes thin-layer placement (TLP) as a strategy for marsh resilience, and National Estuarine Research Reserve System research and recommendations for TLP use.

This paper, published in International Journal of Applied Earth Observation and Geoinformation, describes results of three different mangrove mapping methods to evaluate the impacts of Hurricane Irma, a Category 3 storm that affected southwest Florida in September of 2017. The approach was tested on a very high resolution WorldView-2 satellite image.

This project overview describes a 2015 Collaborative Research project that tested a new strategy to protect coastal habitats in high-energy environments in Florida.

This article, published in Frontiers in Ecology and the Environment in 2018, synthesizes oyster restoration projects since 1964 on the US Atlantic and Gulf coasts and suggests a restoration paradigm to prioritize investment in sites that maximize economic and ecological benefits and minimize construction costs.

This factsheet discusses the potential for gabion-breaks and other living shorelines to dissipate boat wakes and protect shorelines.

This paper, published in Global Environmental Change, assesses outcomes of co-produced science based on an analysis of National Estuarine Research Reserve System funded projects from 1998 to 2014.

This paper, published in Agricultural and Resource Economics Review, stemmed from work completed as part of the Buffer Options for the Bay project in Great Bay, NH.

The joint probability method (JPM) is the traditional way to determine the base flood elevation due to storm surge, and it usually requires simulation of st