Lw. Harding et al., ESTIMATES OF PHYTOPLANKTON BIOMASS IN THE CHESAPEAKE BAY FROM AIRCRAFT REMOTE-SENSING OF CHLOROPHYLL CONCENTRATIONS, 1989-92, Remote sensing of environment, 49(1), 1994, pp. 41-56
Aircraft remote sensing of surface chlorophyll concentrations with NAS
A's Ocean Data Acquisition System (ODAS) was used to determine the sea
sonal and interannual dynamics of phytoplankton biomass in the Chesape
ake Bay from 1989 to 1992. Flights were conducted at a frequency of 1-
2 per week from late winter through early fall, and were scheduled to
coincide with shipboard sampling as weather permitted. The primary sou
rces of in situ data for developing and validating biomass algorithms
were monitoring cruises sponsored by the Chesapeake Bay Program (CBP)
and the NSF-sponsored Land Margin Ecosystem Research (LMER) program of
the University of Maryland. The general approach was to recover estim
ates of biomass from the relationship of surface chlorophyll to the co
ncentration of vertically-integrated chlorophyll weighted bathymetrica
lly. The seasonally and annually specific relations used to estimate b
iomass were then applied to ODAS estimates of surface chlorophyll for
each of >90 flights to produce a time series of total phytoplankton bi
omass (in metric tons of chlorophyll) for the Chesapeake Bay. Estimate
s of algal biomass averaged approximately 500 metric tons, with maximu
m values of 1400 metric tons in spring 1990. These values are in agree
ment with estimates computed from the integrated vertical profiles of
the CBP database using a 3D interpolator model. The total biomass of p
hytoplankton during the spring bloom of 1990 was significantly higher
than in 1989, 1991, and 1992. The causes of these interannual differen
ces are discussed in terms of variations in Susquehanna River flow and
nutrient loading to the estuary.