Water clarity is a measure of how much light penetrates though the water column. Water clarity is dependent upon the amount of particles (e.g. suspended sediment and plankton) and colored organic matter present. Water clarity plays an important role in determining bay grasses and phytoplankton distribution and abundance.
Chesapeake Bay - Indicator Details:
In 2010, water clarity was below the threshold level for the majority of sampling times (score = 0 to 20%; colored red) in most regions of the Bay; a similar pattern was observed in previous years. Water clarity declined in many regions, after improving in 2009. While water clarity has been poor in many regions of the Bay for decades, recent analysis for the report card highlights that many regions, such as the Lower Bay, have been experiencing a long-term decline. The reasons for the long-term decline are still being investigated.
Water clarity was measured at approximately 144 stations up to 14 times during the periods of interest (April to October in the tidal fresh, oligohaline and mesohaline regions, and March to November in the polyhaline regions). Secchi depth is the water depth (in meters) that you can just differentiate black and white quarters of a Secchi disc lowered into the water. The proportion of time that water clarity was below the threshold at each station was calculated and then interpolated to provide estimates between the stations.
This map shows average water clarity (Secchi depth) for Chesapeake Bay and the tributaries from March to November 2010. All Chesapeake Bay tributaries exhibited a gradient in water clarity, with murkier water (shallowest Secchi depth—orange-pink shades) in the mid to upper reaches and clearer waters (deeper Secchi depths—shades of blue) in the lower reaches. The Bay's mainstem exhibited a similar pattern, with murkier water in the Upper Bay and clearer water in the Mid and Lower Bay regions. Lower water clarity in the mid to upper reaches of the tributaries can, in part, be attributed to the mixing of fresh and saline waters leading to a phenomenon known as a turbidity maximum. The bay-wide patterns of water clarity in 2010 seem to be less gradual. For example, there is very little poor clarity in the tributaries and little good clarity in the mainstem. The overall pattern has stayed the same this year as compared to past years, though, with poorer clarity in the tributaries than in the mainstem.
Water clarity was measured at approximately 144 stations up to 11 times during the periods of interest (April to October in the tidal fresh, oligohaline and mesohaline regions, and March to November in the polyhaline regions). Secchi depth is the water depth (in meters) that you can just differentiate black and white quarters of a Secchi disc lowered into the water. Average water clarity (Secchi depth) at each station was calculated and levels between stations were estimated using spatial interpolation software.
Comparison of Bay Health Index scores for 2010 () compared to ()
|0 20 40 60 80 100|
|Lower Eastern Shore (Tangier)|
|Upper Eastern Shore|
|Upper Western Shore|
|Lower Western Shore (MD)|
|Patapsco and Back Rivers|
This figure ranks each region from best to worst water clarity scores for 2010. This figure clearly demonstrates that all regions score moderately to very poorly for water clarity, and are a long way from reaching threshold levels. Following the last two years of moderate improvement, water clarity once again declined in 2010. The Choptank River and Upper Bay regions had the highest water clarity score in 2010, while the Lower Western Shore, the Patapsco and Back Rivers, and the Elizabeth River regions had the lowest (0).
This graph is dynamic, you can: a) show and hide items by clicking them in the legend, b) select year range (click and drag), and c) export as an image.
|Salinity Regime||Season||Relative Status Thresholds (m)*|
* Lacouture et al., Estuaries and Coasts (2006) & Buchanan et al., Estuaries (2005)