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|by Laura Cheshire
May 15, 2000
The Amazon River travels through 6,280 kilometers of rainforest, crossing Peruvian highlands and Brazilian rainforests. Draining approximately 40 percent of the South American continent, the river discharges over 1.5 trillion liters of water daily into the Atlantic Ocean. Throughout its journey, seasonal changes affect its immediate environment and the surrounding land processes. From November to June, rain drenches areas of the Amazon jungle, dropping as much as three meters of water. Much of this deluge runs into the river, and some sections swell to nearly 480 kilometers across, submersing parts of the surrounding forest for up to six months.
Satellite image of the mouth of the Amazon River. (Image courtesy of NASA)
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Amazon discharge is also affected by much larger phenomena, such as periodic El Niño events. During years with an active El Niño, the basin's western (upstream) section receives less precipitation, resulting in less floodplain inundation and discharge downstream.
Examining a large river system like the Amazon is critical to understanding the water cycle. River flow is part of a much larger natural balance in which many other elements interact, including landscape processes, sediment transport, carbon and nutrient cycling, and species ecology. Understanding the impact of river hydrology helps researchers assess the status of an entire basin. However, few scientific tools are available for monitoring river water cycles.
Dr. Charles Vorosmarty and colleagues at the University of New Hampshire investigated the Amazon River drainage basin using satellite data from 1979 to 1985, hoping to develop a method for measuring river flow remotely. In this project, he attempted to demonstrate the potential for applying 37-GHz passive microwave data (obtained from NASA's Pilot Land Data System Archive) to generate remotely sensed river discharge information, using ground-based station data for testing and validation.
In large floodplain-dominated rivers such as the Amazon, variations in water heights create a signal that is detectable by 37 GHz passive microwave radiometers. From these signals, Vorosmarty was able to piece together a picture of river discharge, pixel by pixel, including input from tributaries and periodic differences in water height due to seasonal variations.
Ground-based meteorological station data from the Global River Discharge Database (RivDIS), archived at the Oak Ridge National Laboratory DAAC and the Brazilian Departmento Nacional de Aguas e Energia Eletrica (DNAEE), were used to calibrate and validate hydrology models for the river. From these data, scientists created models from which they could generate a time series of discharge and runoff simulations.
When it came time for ground-truth, Vorosmarty and colleagues found that the satellite imagery and hydrology models agreed. Both data sources reflected the progressive increase in discharge and magnitude, as well as the influence of tributary inflow. Measurements of seasonal high and low water levels also matched. Both also showed interannual variations in discharge caused by the 1982/1983 El Niño event.
Looking to the future of Amazon River research, NASA is scheduled to participate in an international study called Large-Scale Biosphere-Experiment in Amazonia (LBA). Ecology and Hydrology projects sponsored by NASA are designed to support automated data collection along the Amazon from late 1998 to 2003. An important element of LBA is the combination of remote sensing, ground-based measurements, and process modeling. Resulting data from the NASA projects will be archived at Oak Ridge National Laboratory DAAC. Although Amazon data collection continues, funding cuts threaten ground-based river monitoring in many other parts of the world. Consequently, the ability to monitor rivers by satellite will become increasingly valuable and important for scientists attempting to understand river hydrology cycles.
Vorosmarty, C. J., C. J. Willmott, B. J. Choudhury, A. L. Schloss, T. K. Stearns, S. M. Robeson, and T. J. Dorman. 1996. Analyzing the discharge regime of a large tropical river through remote sensing, ground-based climatic data, and modeling. Water Resources Research 32(10): 3137-3150.