Lilia Bartolotta walks with purpose. Slowly, as she breaks through a crunchy top layer and sinks into the snow, but with purpose. The sun is out and some birds are chirping above, but it is certainly cold early this February morning, hovering around freezing.
She’s out to do her river monitoring work, which will allow the Buzzards Bay Coalition to track sources of pollution flowing into our coastal river network, as well as changes in river water level. All are
important metrics to understanding what’s happening within the Buzzards Bay watershed.
This outing has required Bartolotta to put on tall muck boots, as many riverbanks from which she samples water are covered in more than a foot of snow. While in past years, any accumulated snow may have melted before she did her rounds in February; this year, snowbanks pose a little challenge.
One of Bartolotta’s important responsibilities as a Buzzards Bay Coalition Bay Science research assistant is the river monitoring she conducts at 13 locations across the watershed. She travels to her select destinations throughout the year, through snow, rain, and summer heat.
These freshwater sites were chosen because their data elicits how the variety of inputs (i.e. streams, brooks, and rivers) transport pollutants, namely nitrogen, through the watershed and into our monitored embayments. “We have a diverse set of landscapes, from cranberry bogs in the east of the watershed to urban centers to more field-based agriculture in the west,” says Rachel Jakuba, Vice President of Bay Science. “Rivers are major water and nutrient conduits to Buzzards Bay.”
At each site, an app on Bartolotta’s phone downloads data from a sensor that continuously logs water level and temperature at the site. She also does a spot check of the water level by comparing readings with a manual gage, and a temp check with a handheld thermometer.
Water level can be used to calculate yearly patterns in river flow. In the springtime, with high precipitation and (this year especially) a melting snowpack, it is safe to assume that flows will be stronger than they will be in the summer. But from year to year and station to station, how does that flow change? And how does the flow affect how much nitrogen flows to downstream embayments, where the effects are more apparent in murky water, algal blooms, and loss of eel grass?
When she arrives at Angeline Brook, Bartolotta comments that at 35 cm, it is the highest she has ever seen it.