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Location: Watershed-wide analysis – Ipswich Watershed
Purpose: Evaluate the potential for low-impact development (LID) and innovative water conservation techniques to improve base flow within the Ipswich River, if the techniques were applied on a wide, regional basis.
Details: In 2000, the U.S. Geological Survey (USGS) used the Hydrologic Simulation Program--Fortran (HSPF) to develop a watershed-scale precipitation-runoff model of the Ipswich River. The model simulates the watershed’s hydrology and water-use patterns to relate pumping, precipitation, and land use to streamflow (Zarriello and Ries 2000; you can view the full USGS report). In addition to simulating existing conditions, the model may be adjusted to simulate theoretical alternative water pumping and land-use patterns.
To develop a “baseline” to represent current conditions, USGS updated the model published in 2000 to reflect recent changes to pumping patterns in two headwater communities. Specifically, the updated baseline reflects that Reading recently eliminated its Ipswich Watershed withdrawals and began purchasing its full water supply from the Massachusetts Water Resources Authority (MWRA), which derives its water from reservoirs in central Massachusetts. Similarly, Wilmington is reducing its Ipswich Watershed withdrawals by approximately one million gallons per day (MGD) during the summer and replacing this volume with water purchased from the MWRA. All other aspects of the original model remain unchanged for the updated baseline.
A Technical Advisory Committee (TAC) including hydrologists, water suppliers, the Ipswich River Watershed Association, and state and federal agency representatives was convened to determine the theoretical scenarios to be modeled. Streamflow impacts from the following scenarios were modeled:
Watershed Modeling: U.S. Geological Survey
For detailed information on the HSPF model and the modifications made to simulate the scenarios described above, please see the USGS Scientific Investigation Report 2010-5007.
Updated Baseline - Results from the updated model baseline show that eliminating Ipswich Watershed withdrawals by Reading and reducing Wilmington’s withdrawals by one million gallons per day notably improves low-flow conditions in the Ipswich River, most significantly in the headwaters adjacent to the Reading and Wilmington wells.
Build-Out – The build-out simulation resulted in negligible additional impacts to streamflow for most of the tributaries and stream reaches in the watershed. The largest impact was observed in a stream that drained substantial amount of undeveloped land that is zoned for industrial and commercial land uses. For this stream, the build-out condition resulted in higher high flows (more flooding, scouring, and erosion) and lower low flows compared to current conditions. The reason that so little impact was observed from the build-out scenario for most of the watershed is due to the fact that most of the developable land in the watershed is zoned for low-density housing, which tends to have little effective impervious area. Therefore, the build-out condition does not represent a substantial change in effective impervious area over the whole watershed, relative to today’s conditions.
It’s important to note, however, that while the model indicates that streamflows in major tributaries and the mainstem are unlikely to be directly impacted from new development, streamflows are very likely to be indirectly affected, if the water demand from the new development is met with Ipswich Watershed sources, which will increase pumping beyond the current rates. Additionally, the model was not able to account for decreases in water quality that may results from build-out conditions.
LID Retrofit – The LID retrofit simulation similarly resulted in negligible improvements to streamflow conditions in the major tributaries and stream reaches. The stream reach most dramatically affected by simulated LID retrofits drains a portion of the upper watershed that has a high percentage of effective impervious area (22%), due to the presence of lots of commercial and industrial parcels. For this stream, a 50% reduction of impervious area in the vicinity led to decreased high flows (less flooding, scouring, and erosion) and higher low flows (the retrofits eliminated periods of time when the riverbed would go dry). Most of the other tributary and stream reaches drain areas with effective impervious areas of 9% or less. These levels of effective impervious area are low enough that a reduction by half does not amount to a large absolute change in watershed flow conditions.
Water Conservation Scenario – The simulated reductions in town-wide pumping, ranging from 1.4% to 8.5%, reflective of the hypothetical wide-spread adoption of the pilot water conservation strategies had very modest effects on flows in the tributaries and mainstem reaches. By comparison, a simulated reduction of 20% at all public water supply withdrawal sources in the watershed resulted in a slightly more measurable mitigation of extremely low flows. In sharper contrast, the simulated ceasing of all public water withdrawals in the watershed resulted in dramatic improvements in streamflow in many tributaries and mainstem reaches.
Local-scale land use simulations – The local scale modeling demonstrated that small streams in the vicinity of parcels that undergo significant development undergo substantial impacts to flow conditions. The conversion of the 100-acre parcel from forest to commercial land use dramatically increased flood flows and caused severe low flows. Conversion of the forest to low-density or high-density housing increased flood flows somewhat, but tended to raise the volume in the stream during low-flow periods, too. This can be attributed to the clearing of trees, which soak up groundwater during the growing season. Since residential landscapes draw less water from the subsurface groundwater stores than forests do, groundwater contributions to streamflow can actually increase when forests are converted to residential development.
The local scale simulation series also investigated the impact of clustering development on a portion of the lot and preserving the natural forest on the area that remained. In most cases, clustering succeeded in significantly reducing the impacts to streams caused by more uniform development. Lastly, the local scale simulation explored the influence of natural geology on the above trends, and the results suggest that land use changes that occur over subsurface conditions dominated by sand and gravel tend to cause more significant disruptions to natural streamflow than land use changes over subsurface conditions dominated by glacial till. As a result, introducing LID to mitigate the streamflow impacts of development makes a more substantial difference in areas dominated by sand and gravel.