16 September 2011
Hurricane Irene passed this way two weeks ago, and dumped a lot of rain on the mid-Atlantic region and the northeast. As a result, runoff increased, rivers swelled, and sediment was mobilized. Some of that sediment was suspended and transported downstream. On Tuesday, I got this e-mail from my colleague Ken Rasmussen, who took students out on an oceanography field trip to Chesapeake Bay a week after the storm:
Was out with students on bay on 9/11. Turbidity was amazing- more like chocolate milk. Lots of logs, trees, floating urban debris, etc. Mid-bay surface salinity remarkably low (less than 4 ppt; more typical is 16 ppt in Sept.). Thought you’d like to see this MD DNR satellite image and mid-bay surface photo, both attached. On the bright side- dead zone was mixed/disrupted.
NASA Earth Observatory published a better version of the satellite image than the MD DNR version, so I’ll reproduce a portion of it here:
Here’s Ken’s on-the-scene photograph:
It seemed to have a bluish tinge to it, so I clicked “Auto Levels” in Photoshop, and got this result:
That’s a lot of suspended sediment!
Just thought I’d share this, with Ken’s permission, of course. It makes me think about the role of hurricanes and other infrequent events in the sedimentary record. The salinity change (due to the large influx of freshwater runoff) is interesting too. Does that have any effect on sedimentation rates? I’m thinking about charges on the surface of clay particles, and flocculation rates changing due to the decrease in ions in the seawater – just wondering aloud here. I know next to nothing about those sorts of geochemical/geophysical interactions. Chime in if you can enlighten me.