Title: Operational AVHRR based Monitoring of Central American Volcanoes
1Operational AVHRR based Monitoring of Central
American Volcanoes
M. J. Wooster (KCL), J.A. Saballos, W. Strauch,
K. Dill (INETER) P. and J. Stephenson (BURS)
2Operational Remote Sensing system
- Operational test of previously derived technique
- Design a AVHRR system to monitor volcanoes in
real time - Examine both the usefulness of the system for
volcano monitoring and the dissemination of such
data into the local communities for volcanic
hazard and early warning - Funding for project
- DfID grant - 2½ year project
3AVHRR and Thermal Monitoring?
- AVHRR Advanced Very High Resolution Radiometer
- NOAA operates the POES series, upon which the
AVHRR sensor is mounted. - Orbit at 850 km.
- Scans through ? 55 either side of the orbital
track - 5 spectral channels .
- For thermal monitoring, Channels 3 and 4 are most
useful. - As surface temperatures rise, the thermal
emmittance increases much more rapidly in the MIR
than in the TIR - Important as at the resolution of the AVHRR, the
areas of the volcano at highly elevated
temperatures are likely to be highly sub-pixel - Possible for to detect these increases over and
above the ambient background emission, even
though the hot area may comprise less than 0.1
(i.e. 1000th) of the pixel area.
4AVHRR Real time Volcano Monitoring Project
- Objectives
- To investigate the potential improvements to
local volcano monitoring and hazard mitigation
operations that can be gained via use of locally
captured satellite remote sensing data in
developing countries. - The project includes both physical and social
science components in order to make this
assessment, and the main data used is from AVHRR,
captured locally in Nicaragua. - Ideal Accomplishments
- Installation of AVHRR receiving station in
Nicaragua (INETER). - Design and operation of fully automated data
capture and pre-processing system. - Extensive case studies into the application of
AVHRR to monitor and detect thermal volcanic
activity. - Design of automated analysis system to monitor
volcanoes in Nicaragua, Guatemala, El Salvador
and Costa Rica. - Development of web based interface for data
download and thermal monitoring by outside
geo-science organisations. - Investigation of auto email alerts based on AVHRR
signals - First test of an operational system in developing
country - Involves local volcanologists and Increased
application of data and results. - Other systems in US and Japan
5AVHRR Receiving Station and Data
- Image area 2600 km 2600km
- 6 - 8 satellite passes per 24 hours (day and
night imagery) - Much more than the single daytime image online at
the SAA, operated by NOAA. - Data
- 5 Spectral Channels
- Measuring Reflectance and Temperature
- At 1.1 km resolution at nadir
- Analysis
- Use T3 T4 to quantify at volcanic activity
- T3 increases rapidly in presence of sub pixel
hotspot - Determine radiance anomalies for the hotspot
pixels - Use T4 T5 for ash cloud test
- Provide time series of important data and
automated alerts
6Computing/Data Storage
- Computing
- Data Capturing
- Data Analysis
- Software
- BURS
- ENVI/IDL
- Data files
- RAW 10 40 MB
- ENVI BIL 90 180 MB
- Data Storage
- Per day 400 500 MB
- CD backup
- Copied each week
- Storage within INETER
- Development to DVD storage
- Analysis outputs
- Stored on PC
- Displayed on website
7Number of AVHRR passes?
- 16th January 2005
- 9 passes successfully captured
- 17th January 2005
- 7 passes successfully captured
8Volcanoes analysed by the AVHRR monitoring system
- Nicaragua
- Cerro Negro, Concepcion, Cosiguina, Masaya,
Mombacho, Momotombo, San Cristobal, Telica - Guatemala
- Acatenango, Atitlan, Cerro Quemado, Fuego,
Pacaya, Santa Maria/Santiaguito, Tacana,
Tecuamburro - El Salvador
- Izalco, San Miguel, San Salvador, Santa Ana
- Costa Rica
- Arenal, Irazu, Poas, Rincon
9Planning orbits
Downloads orbit element data daily from NOAA and
uses this to accurately predict the next
satellite overpass time and position
10AVHRR Capture System
- Data Capture
- Data calibration
- Data converted to universal format
- Pre-processing fully automated
- NOAA Scheduler
- Carries out orbit planning, data capture and data
calibration - Conversion to universal format automated
11Analysis System Summary
- Uses IDL/ENVI
- Automatically compiles and runs code if satellite
pass within past 45 minutes - If no pass, then will close and re-load in 45
minutes - Loads AVHRR scene into ENVI and extracts the
following data - Channels 1 to 5, Latitude and Longitude
- Satellite Azimuth, Satellite Elevation, Sun
Azimuth and Sun Elevation - Image covers 8 volcanoes in Nicaragua, 8 in
Guatemala, 4 in Costa Rica and 4 in El Salvador
(not necessarily all at once) - Uses image geocoding to find the pixel
corresponding to the volcano summit - Possible geo-location uncertainty of a few
pixels. - For each volcano, program carries out the
following analyses - Find the Max T3 T4 close to the identified
summit pixel - Determines thresholds to detect hot/anomalous
pixels on volcano - Determines radiance anomalies at these anomalous
pixels - Carries out cloud analysis of region surrounding
the volcano
12Volcano Activity Identification Stage 1
- Finds the Maximum T3 T4 value in a 7 by 7 grid
around the summit pixel. This is the updated
volcano summit location. - Determines this to be the location of the volcano
and then selects a 7 by 7 grid around this. - Determines the mean and standard deviation of
this new array - Analyses the grid to determine which pixels are
anomalous. If none, then no further radiance
calculations - If some then uses these anomalous pixels in
radiance calculations
13Radiance Calculations Stage 2 (a)
- Calculates the Radiance for Channels 3, 4 and 5
from Planck equation - ? wavelength (m) T is temperature (K)
- L is Spectral Radiance (W/m2/sr/µm) h is
Plancks Constant (6.610-34 Js) - k is Boltzmanns constant (1.3810-23 J/K) c
is the speed of light (3108 m/s) - Background Radiance Anomaly
- Difference between AVHRR T3 and the surrounding
non-thermally anomalous background pixels in the
same spectral channel, T3. - The advantage
- Effect of the atmosphere on the radiance anomaly
measure should be minimised - The disadvantage
- Value of the retrieved thermal anomaly effected
if hotspot and background pixels at different
elevations
14Radiance Calculations Stage 2 (b)
- Equivalent Radiance Anomaly
- Difference between the AVHRR T3 signal and the
simulated T3 signal modelled using the T4
observations at those same pixels using the
Planck function. - The advantage
- Effect of differing elevations on the radiance
anomaly is largely avoided - The disadvantage
- Differences in the atmospheric effect between T3
and T4 can affect the radiance anomaly
calculations, - May also be underestimated if the volcanic
hotspot significantly effects the T4
observations. - Simulated Radiance Anomaly
- Calculate the empirical linear best-fit
regression relationship between the AVHRR T3 and
T4 data around the volcanic hotspot - This relationship is then used with the AVHRR T4
data of the volcanic hotspot pixels to simulate
the AVHRR T3 signal at these locations would be
in the absence of the volcanic hotspot. - These simulated T3 observations are then
subtracted from the actual MIR observations to
calculate the observed volcanic thermal anomaly. - Advantage
- Allows for a difference in atmospheric effect
between T3 and T4. - Disadvantage
- Only works if a strong regression relationship is
found between these two channels in the
background data selected.
15Outputs from Analysis (1)
- Text file based outputs for each volcano
- Channels 1 to 5 at summit and hotspot
- Channels 3 4 and 4 5 at summit and hotspot
- No of Ash and saturated pixels
- Three radiance anomalies
- Distance between summit and hotspot
- CI and cloud value for summit pixel
Cloud index Summit value
Radiance anomalies
Date and time of image
Channels 3, 4 and 5 at hotspot
16Outputs from Analysis (2)
- Fully georeferenced images for each country and
volcano - Processed data in real-time for own personal
analysis - Gridded text files of AVHRR data for each volcano
- Time series plots of text data.
- Data sent automatically by FTP to web server
- ARCVIEW data for each country and each volcano
- ENVI image data for each country and each volcano
- ENVI GIS shape files for each country and each
volcano - Georeferenced imagery for each country and each
volcano - Time series text files for each country and each
volcano - Time series figures for each country and each
volcano
17Georeferenced Imagery for Nicaragua
Cerro Negro
18Georeferenced Imagery for Guatemala
Fuego
19Georeferenced Imagery for El Salvador
Izalco
20Georeferenced Imagery for Costa Rica
Poas
21Threshold Analysis
- Uses predefined thresholds to determine volcano
alert level - Four Levels. Maximum 3, Minimum 0
- Threshold levels for Equivalent Radiance anomaly
- Level 0 1 1.6 W/m2/str/µm
- Level 1 2 3.2 W/m2/str/µm
- Level 2 3 6.4 W/m2/str/µm
- Reads in the AVHRR Channel and Radiance anomaly
time series for the volcano - Determines if the Cloud Index gt 0.6 or if it is a
daytime pass. - Determines if the Radiance anomaly has passed
over the predefined threshold for the volcanos
alert level - Counts the total number of alerts in the past 15
images - If 2 or more than volcano alert level rises
- If less than 2 than volcano alert level stays the
same - If 3 or more times below threshold then alert
level drops - If Radiance anomaly has passed over threshold
data is written to text file for attachment to
e-mail. - Equivalent Radiance anomaly
22E-mail alert system
- Data written as text to a .txt file for
attachment to an e-mail - Uses a e-mailing software and a batch file to
auto email to a mailing list for the country,
based on the volcano. - Mailing lists for each country.
- avhrr_gua_at_gf.ineter.gob.ni
- avhrr_nic_at_gf.ineter.gob.ni
- avhrr_sal_at_gf.ineter.gob.ni
- avhrr_cor_at_gf.ineter.gob.ni
- e.g. Nicaragua, for each of the eight volcanoes
monitored an e-mail is sent to the
avhrr_nic_at_gf.ineter.gob.ni list if the volcano
has passed the defined thresholds.
- 3 alert level changes
- 6 e-mails sent
23Example of E-mail Alert
24Real-time data accessible from website
http//sat-server.ineter.gob.ni/
- Fully georeferenced imagery ENVI Image files
- Time series of Radiance anomalies E-mail alert
system - Gridded data around each volcano
25Summary
- AVHRR system analyses for 24 volcanoes across
Central America - AVHRR can detect and monitor the thermal
signature of volcanic activity in real time - System analyses for thermal activity of the
volcanoes - System is fully automated
- Capture
- Analysis
- Automated E-mail alert for all volcanoes
- Website interface interface to thermal analysis
for 24 volcanoes, 24 hours per day - Automatically updated
Developments
- Improvement and automation of ash cloud detection
- Reduction in time to send data to FTP server
- Most recent 3 5 images displayed on website