We would like to thank Andrew Peresta for deploying and maintaining the EXO2 sonde at the Kirkpatrick Marsh creek and the entire MARSHCYCLE team for many thoughtful discussions. We would also like to thank two anonymous reviewers for comments that helped greatly improve this
manuscript. This research was supported by National Aeronautics and Space
Administration grant NNH13ZDA001N-CARBON. Contact the
corresponding author for model forcing and output and post processing scripts.This is University of Maryland Center for Environmental Science contribution # 5392.
Electronic supplementary material
Fig. S1
(a) Unfiltered fDOM and (b) depth for the entire sampling period in 2015.
Gaps in the data indicate periods when the EXO-2 Sonde was not deployed.
(DOCX 110 kb)
Fig. S2
Conceptual diagram of the estuarine surface gradient progression during a
“typical” wind progression in the Rhode River, MD in the spring and fall. As southerly winds blow a barotropic surface pressure gradient sets up in the back of the Rhode River depicted by the H in (a) that forces water back towards the marsh, depressing flow out of the wetland depicted by the shaded region. As Northwesterly winds progress, local wind driven flow enhances flow out of the creek back towards the marsh, while local wind effects set up a low pressure in the back and mouth of the Rhode River, depicted by the L’s (b). (DOCX 145 kb)
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