USING NEURAL NETWORKS TO ASSESS THE INFLUENCE OF CHANGING SEASONAL CLIMATES IN MODIFYING DISCHARGE, DISSOLVED ORGANIC-CARBON, AND NITROGEN EXPORT IN EASTERN CANADIAN RIVERS
Ta. Clair et Jm. Ehrman, USING NEURAL NETWORKS TO ASSESS THE INFLUENCE OF CHANGING SEASONAL CLIMATES IN MODIFYING DISCHARGE, DISSOLVED ORGANIC-CARBON, AND NITROGEN EXPORT IN EASTERN CANADIAN RIVERS, Water resources research, 34(3), 1998, pp. 447-455
Changes in both air temperature and precipitation are expected as atmo
spheric CO2 increases because of anthropogenic activities. These chang
es will not be evenly distributed across seasons because of the comple
xity of climate patterns. Using climate, hydrology, and water chemistr
y data, we investigated how changes in the seasonal climates of the At
lantic Provinces of Canada would change both hydrology and geochemical
cycling of 14 river basins influenced by wetlands. We calculated mont
hly discharge (Q) and dissolved organic carbon (DOG) and dissolved org
anic nitrogen (DON) exports from 1983 to 1992 and developed three neur
al network models relating climate variability to hydrologic and geoch
emical fluxes from the basins. We then identified a series of potentia
l temperature/precipitation scenarios which we applied to the models.
We then studied how changes in climate regimes would affect water disc
harge and aquatic dissolved carbon and nitrogen released from these ba
sins. Our results predict a complex series of possible outcomes for wa
ter and elemental fluxes. Warming or cooling in each season combined w
ith potential changes in precipitation will cause completely different
outcomes as snowpack melting dominates winter and early spring condit
ions and evapotranspiration controls summer and fall. A warming winter
would cause less snow storage and more runoff, with little evapotrans
piration. Warmer summers, on the other hand, will be influenced by eva
potranspiration, and water flows will be lower. Carbon and nitrogen ex
ports from basins generally mirror those of Q. Our results suggest tha
t major hydrological changes in basins may lead to significant ecologi
cal and water resource impacts, especially in the spring and early sum
mer.