| Biological Sciences | Research
and Technology 2002
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| Spatial
Rainfall Monitoring and Analysis at KSC and CCAFSFrom 1989 to 2000 |
NASA and various agencies have monitored rainfall at KSC since 1983 to evaluate long-term trends in precipitation, deposition, weather forecasting, and tropical storms. These sites have been operated and maintained by:
The spatial rainfall patterns on KSC are important for a variety of reasons. The lagoonal volumes are controlled by direct precipitation on their surfaces plus runoff and surface input from point and nonpoint source discharges, plus or minus groundwater seepage, minus evapotranspiration, plus or minus flow through Haulover Canal, plus or minus tidal exchanges with the Atlantic Ocean. The rainfall patterns will have to be considered in the further growth on KSC for roads and facility siting criteria and runoff patterns of the major watersheds. This could impact the outfall of stormwater runoff to the Banana River, Indian River, and Mosquito Lagoon, which border the east, west, and north of KSC. |
This freshwater could impact the salinity and nutrient levels of the rivers, which could influence the sea grass distributions. This could impact the fish nurseries and the feeding grounds of the endangered manatees. The rainfall patterns on the land could also affect the primary production of biomass and food for other endangered species (Florida scrub-jay and indigo snake). Another effect could be on the fine-fuel moistures on the various prescribed burn units for any given year, which might hinder the necessary burn cycles for proper habitat maintenance.
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Mean Spatial Rainfall Pattern at KSC and CCAFS 1989 to 1995 and From 1998 to 2000 |
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