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Summary
BCI (9°10'N, 79°51'W) is an island which was isolated
from the surrounding mainland in 1914 following the damming of the
Chagres river and the formation of Gatun Lake. The island, rising
137m above Lake Gatun, has an area of 1500 ha which are covered by
forest that has remained relatively undisturbed for at least 100
years. BCI forms part of the Barro Colorado Nature Monument (BCNM).
For more information about STRI facilities on BCI and the BCNM
click here
The island receives an average of 2623 mm of rain per year.
Day-time temperatures reach an average of 32°C, with night-time
lows of approximately 23°C. The meteorological year is divided into
two parts: a pronounced dry season (approximately from mid-December
to the end of April), and a wet season (May to mid-December). On
average, only 285 mm of rain falls during the dry season. Relative
humidity, soil moisture, air pressure, solar radiation,
evapotranspiration, wind speed and direction all show marked
wet/dry season differences. On the other hand, temperature varies
relatively little throughout the year.
There are three Physical Monitoring Stations on BCI: The
Clearing (‘El Claro’), the Lutz Watershed Weir, the Lutz Tower and the Conrad Weir.
Data are collected using two different methods:
electro-mechanical (electronic sensors, data loggers, chart
recorders, etc.), and manual (rain gauges, max-min thermometers,
sling psychrometers, soil samples, etc.) by a technician. In
general, manual measurements have shown themselves to be the
most accurate over the long-term. Wherever possible,
parameters are measured both manually and electronically. The only
exceptions to this rule are solar radiation (electronic only),
estimated evapotranspiration (manual only), and gravimetric soil
moisture (manual only).
For a summary of the most recent data collected, plus long-term averages report, please click on the following link:
Yearly_Reports_Barro_Colorado_Island
Monthly summaries_BCI_horizontal
Monthly summaries_BCI_vertical
Special El Niño 2015/6 analysis: 2015_16 El Niño Analysis.xlsx
Clearing
The Clearing (or ‘El Claro’ as it is know on the
island) is a small grass-covered clearing located between the edge
of the forest and the foundations of several former laboratory
buildings. The station was established in 1972 and was the original
meteorological station managed by STRI. An older station
(established in 1929 and operated by the Panama Canal Authority) is
located near to the shore of Lake Gatun.
The Clearing station records both manual and electronic (tipping bucket)
precipitation, manual and electronic temperature and humidity,
electronic barometric pressure, as well as manual potential
evapotranspiration (EtGage atmometer).
Sensors
Sensor manuals in .pdf format are available for download
here.
Electronic Data Download
Manual Data Download
Metadata Download
Metadata_BCI.txt
Lutz Watershed and Meteorological Tower
The Lutz catchment is probably typical of the many small, steeply-sloped catchments draining away from the center of the island. It is located immediately east of the laboratory clearing. The steeply sloped (20-30°) catchment drains an area of 9.73 ha. The forest covering the catchment was mostly deforested during the construction of the Panama Canal around the turn of the century, but since then it has been allowed to regenerate.
Built in 1972, the Lutz tower was originally 42m in height. In October of 2001 the tower was raised to 48m due to the increase in height of the surrounding forest that happened during the previous 30 years.
The station consists of a vertical meteorological transect through the forest canopy with temperature/humidity sensors at 1, 20, 42 and 48m. . There are solar radiation sensors, an anemometer and an EtGage atmometer on the uppermost level of the tower. Manual measurements of max/min temperature and noon-time relative humidity are taken at the Lutz tower as well.
Gravimetric soil moisture samples are made at ten locations around the Lutz catchment. Soil samples are made at 0-10cm and 30-40cm at each location. Samples are taken every two weeks during the period June to November and weekly from December to May.
The V-notch weir located near the base of the tower measures the run-off from most of the Lutz creek catchment. Data are recorded using both a chart recorder and a pressure-base bubbler. Daily height recordings are made by a technician for calibration purposes.
Sensors
Sensor manuals in .pdf format are available for download
here.
Electronic Data Download
Parameters |
Frequency |
Units |
Downloads |
Air Temperature 1m (max, min, average) |
15 min |
Celsius |
Barro Colorado Island, Lutz Tower 1m_Air Temperature
|
Air Temperature 20m (max, min, average) |
15 min |
Celsius |
Barro Colorado Island, Lutz tower 20m_Air Temperature
|
Air Temperature 42m (max, min, average) |
15 min |
Celsius |
Barro Colorado Island, Lutz tower 42m_Air Temperature
|
Air Temperature 48m (max, min, average) |
15 min |
Celsius |
Barro Colorado Island, Lutz tower 48M_Air Temperature
|
Relative Humidity 1m (max, min, average) |
15 min |
% |
Barro Colorado Island, Lutz tower 1m_Relative Humidity
|
Relative Humidity 20m (max, min, average) |
15 min |
% |
Barro Colorado Island, Lutz tower 20m_Relative Humidity
|
Relative Humidity 42m (max, min, average) |
15 min |
% |
Barro Colorado Island, Lutz tower 42m_Relative Humidity
|
Relative Humidity 48m (max, min, average) |
15 min |
% |
Barro Colorado Island, Lutz tower 48m_Relative Humidity
|
Solar Radiation Flux (max, min, average) |
15 min |
w/m2 |
Barro Colorado Island, Lutz tower 48m_Solar Radiation, Pyranometer
|
Wind Direction 45m (vect mean, std. deviation) |
15 min |
degrees |
Barro Colorado Island, Lutz tower 42m_Wind direction
|
Wind Direction 48m (vect mean, std. deviation) |
15 min |
degrees |
Barro Colorado Island, Lutz tower 48m_Wind direction
|
Wind Speed 42m (max, min, mean horiz speed) |
15 min |
km/hr |
Barro Colorado Island, Lutz tower 42m_Wind speed
|
Wind Speed 48m (max, min, mean horiz speed) |
15 min |
km/hr |
Barro Colorado Island, Lutz tower 48m_Wind Speed
|
Runoff Lutz Creek (level, flow-rate, discharge) |
5 min |
m3 |
Barro Colorado Island, Lutz Catchment_Runoff |
Manual Data Download
Parameters |
Frequency |
Units |
Downloads |
Temperature 1m (Daily Max/Min) |
daily |
Celsius |
Barro Colorado Island, Lutz tower 1m_Air temperature, manual |
Temperature 42m (Daily Max/Min) |
daily |
Celsius |
Barro Colorado Island, Lutz tower 42m_Air Temperature, manual |
Temperature 48m (Daily Max/Min) |
daily |
Celsius |
Barro Colorado Island, Lutz tower 48m_Air Temperature, manual |
Evapotranspiration 42m |
daily |
cm |
Barro Colorado Island, Lutz tower 42m_Potential Evaporation |
Evapotranspiration 48m |
daily |
cm |
Barro Colorado Island, Lutz tower 48m_Potential Evaporation |
Relative Humidity 1m |
daily |
% |
Barro Colorado Island, Lutz tower 1m_Relative Humidity, manual |
Relative Humidity 20m |
daily |
% |
Barro Colorado Island, Lutz tower 20m_Relative Humidity, manual |
Relative Humidity 42m |
daily |
% |
Barro Colorado Island, Lutz tower 42m_Relative Humidity, manual |
Relative Humidity 48m |
daily |
% |
Barro Colorado Island, Lutz tower 48m_Relative Humidity, manual |
Soil Humidity – Lutz Creek
H2O by wet, H2O by dry
|
1-2 weeks |
% |
Barro Colorado Island, Lutz catchment, Soil moisture, manual |
Conrad Weir
The Conrad catchment is a more gently sloped catchment draining much of the central area of the island, including most of the 50-ha plot. The catchment is approximately 40.2 ha in size. Unlike the Lutz catchment, the forest covering the catchment was not cut during the construction of the Panama Canal.
The weir experienced several stages of development between 1993 and 1996 as additional height and wings were added to accommodate all stages of the Conrad stream. The weir consists of a 90 degree ‘V’ set into a two-stage rectangular weir. Data are recorded by a pressure-based bubbler.
Please read our data use policy before using any data from this page.
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