More Like this

1. Data-driven modeling of wind waves in upper Delaware Bay with living shorelines

   https://doi.org/10.1016/j.oceaneng.2022.111669  

   Wang, Nan; Chen, Qin; Zhu, Ling; Wang, Hongqing (August 2022, Ocean Engineering)
2. Organic Signatures of Surfactants and Organic Molecules in Surface Microlayer and Subsurface Water of Delaware Bay

   https://doi.org/10.1021/acsearthspacechem.2c00220  

   Burdette, Tret C.; Bramblett, Rachel L.; Deegan, Ariana M.; Coffey, Nicole R.; Wozniak, Andrew S.; Frossard, Amanda A. (December 2022, ACS Earth and Space Chemistry)
3. Metagenomes, Metatranscriptomes, and Metagenome-Assembled Genomes from Chesapeake and Delaware Bay (USA) Water Samples

   https://doi.org/10.1128/mra.00262-21  

   Ahmed, Mir Alvee; Lim, Shen Jean; Campbell, Barbara J. (May 2021, Microbiology Resource Announcements)

   Newton, Irene L. (Ed.)

   ABSTRACT Here, we present 36 metagenomes, 59 metatranscriptomes, and 373 metagenome-assembled genomes (MAGs) from Chesapeake and Delaware Bay water samples. This data set will be useful for studying microbial biogeochemical cycling in estuaries. 

   more » « less
4. Understanding the dynamic response of Durafet-based sensors: A case study from the Murderkill Estuary-Delaware Bay system (Delaware, USA)

   https://doi.org/10.1016/j.ecss.2023.108247  

   Gonski, S. Fisher; Ullman, William J.; Pettay, D. Tye; Booksh, Karl S.; Martz, Todd R.; Luther, George W.; Cai, Wei-Jun (April 2023, Estuarine, Coastal and Shelf Science)
5. Formation of sea ice ponds from ice-shelf runoff, adjacent to the McMurdo Ice Shelf, Antarctica

   https://doi.org/10.1017/aog.2020.9  

   Macdonald, Grant J.; Popović, Predrag; Mayer, David P. (September 2020, Annals of Glaciology)

   null (Ed.)

   Abstract Ponds that form on sea ice can cause it to thin or break-up, which can promote calving from an adjacent ice shelf. Studies of sea ice ponds have predominantly focused on Arctic ponds formed by in situ melting/ponding. Our study documents another mechanism for the formation of sea ice ponds. Using Landsat 8 and Sentinel-2 images from the 2015–16 to 2018–19 austral summers, we analyze the evolution of sea ice ponds that form adjacent to the McMurdo Ice Shelf, Antarctica. We find that each summer, meltwater flows from the ice shelf onto the sea ice and forms large (up to 9 km 2 ) ponds. These ponds decrease the sea ice's albedo, thinning it. We suggest the added mass of runoff causes the ice to flex, potentially promoting sea-ice instability by the ice-shelf front. As surface melting on ice shelves increases, we suggest that ice-shelf surface hydrology will have a greater effect on sea-ice stability. 

   more » « less