| |
Project Amazonia: Monitoring - Water
River Flow Volume
Monitoring of river volume is important as a means of
calibrating hydrologic cycle models. It is also important in order to
predict and give advance warning for floods further downstream.
Monitoring
|
Acoustic Doppler Current Profiler (ADCP): device which uses
ultrasonic device to monitor river volume
|
|
Interferometric synthetic: remote sensing techniques that
collects data on river volumes
|
|
Airborne Scanning Laser Altimetry (LiDAR): detect water level
changes. This technique has already proven to be highly useful for measuring
vegetation height and so data from such a system would be particularly
useful in modeling runoff.
|
Groundwater
One major source of threats is the mining processes and
their side effects. Acid mine dragains (or AMD) is a solution originating at
a mine site and carried off in rain or surface water.
Monitoring
| Thermal imaging cameras on the planes (part of
SIVAM’s data collection system): can locate groundwater flows (but not
useful in determining chemical composition) |
| Quanta-G water quality instrument: designed
specifically for ground water monitoring. It measured temperature specific
conductance, salinity, total dissolved solids, dissolved oxygen reduction
potential, depth, and vented level. |
Rainfall
| Infrared Remote Sensing: High frequency monitoring,
use only information of cloud-top temperature to determine surface
rainfall |
| Microwave Remote Sensing: Based on the distribution
of within the cloud, explain instantaneous rainfalls more realistically,
but can only monitor twice/day for any location, Housed on low-orbiting
satellites |
| Fixed-time Recording Local Sensing: Records the
amount of rainfall over a set interval of time. In some ways this is a
very inefficient method as it produces a large number of extraneous zeros
in the data set |
| Fixed-event Recording Local Sensing: Fixed-event
recording records the time interval over which a set amount of rain falls.
The method eliminates the large amount of extraneous zeros, making date
sets leaner and more manageable. |
| Climate Prediction Center merged analysis of
precipitation (CMAP): The merged analysis was composed of two kinds of
data – standard precipitation (STD) and enhanced precipitation (ENH). STD
consisted of gauge observations, where as ENH consists of five kinds of
satellite estimates. |
Evapotransportation
| Direct (Lysimeter): evapotransportation =
precipitation-drainage-mass |
| Indirect (Water Balance): Lysimeters (even though
accurate) is not effective on a large scale. Therefore, even though it is not
as accurate, we use indirect method to determine evapotranspiration.
|
Fish
Sedmientology
Each year the Amazon transports suspended sediment to the
delta plain. The combined exchanges of sediment are estimated an average of
2070Mt per year.
Monitoring
| Optical Backscatter: shines light into a sample volume
and measures reflected light using photodiodes positioned around the emitter.
|
| Acoustic: Emits short bursts of high frequency sound
from a transducer. The sediment will reflect a certain amount of the sound
depending upon the concentration, particle size and frequency. |
| Spectral Reflectance: Suspended sediment concentrations
are measured using the amount of radiation reflected from a body of water and
the properties of that water. |
| Digital Optical: A charged-coupled device records the
sediment/water mixture in-situ. It can be analyzed for size and concentration
of suspended sediment particles, and to confirm the nature of the sediment.
|
Next: Flora ->
|