This document discusses using moderate resolution MODIS satellite data at high resolutions by calculating the observation footprints in polygon format rather than relying on the predefined grid. The authors simulate MODIS data over a study area in Hungary by taking the mean of high resolution SPOT satellite data within each MODIS observation footprint. They compare simple gridding versus assigning values to crop parcels based on the proportion of pixels within each. Their quality assessment shows correlation and errors are higher when using parcel-based approach versus gridded data, indicating moderate resolution data can provide high resolution information when using observation footprints rather than the grid.
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Pushing MODIS to the edge: high-resolution applications of moderate-resolution data
1. Pushing MODIS to the edge:
High-resolution applications of
moderate-resolution data
Dániel Kristóf – Róbert Pataki –
András Kolesár – Tamás Kovács
MultiTemp 2013 | Banff, AB, Canada, 25-27 June 2013
Institute of Geodesy, Cartography and Remote Sensing
Budapest, Hungary
2. Outline
MODIS at a glance
Beginning
Expectations and observations
Particularities of MODIS data
New preprocessing approach & first results
Current state
Time series construction and quality measures
Results achieved so far
Conclusions and outlook
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3. MODIS
Moderate Resolution Imaging Spectroradiometer
Onboard NASA’s Terra&Aqua satellites
36 spectral bands between 0.405 and 14.385 micrometers
Wide field of view, daily (or even more frequent) coverage
with nominal nadir resolutions of 250, 500 and 1000 meters
Sophisticated operational data processing (MODAPS)
A large number of preprocessed data & scientific products
available (for free…), timeliness
Well-published algorithms, systematic revision and
reprocessing (also backwards processing; Currently:
„Collection 5”)
An archive continuous in time: (almost) gapless data since
1999!
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4. Beginning: initial motivation…
A user wants to detect the date of interventions on
agricultural fields, size comparable to a 250-m MODIS pixel
Band 2
Band 2,
QC 4096
(OK)
4
5. Beginning: initial motivation…
Terra MODIS land
surface reflectance
Day x+1
Day x+1
Aqua MODIS land
surface reflectance
Day x
Day x
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7. Why…? MODIS particularities:
– Gridding artifacts:
• Data stored in a predefined grid, resampled
• Average overlap between observations and
their respective grid cells less than 30% [Tan et
al., RSE 105(2006):98-114]
– Problems with the raster data model itself:
• Fixed size and orientation of the cells although
the observation dimensions vary across the
scene due to the wide field of view (+/- 55
degrees), orientation definitely not N-S
• The grid cells / pixels do not represent the area
where the signal is originated from
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9. Proposed solution
• A possible solution would be the spatial and/or temporal
compositing and/or filtering, but: loss of resolution and
information…
• Our approach: Change data representation
– Calculate and store observation footprints in polygon format
– Each polygon represents the respective observation footprint (“real
pixel”) sensed during image acquisition
• Geolocation datasets (MOD/MYD03) contain all necessary
info to do this
– Ground location, dimensions and orientation of each MODIS pixel
footprint can be determined from:
Latitude, Longitude, Height, Sensor Zenith Angle, Sensor Azimuth
Angle, Slant Range
– Geolocation accuracy: 50 m at 1 sigma at nadir
– Swath images (MOD/MYD02) or „backsampled” Surface Reflectance
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11. First results: correlation with SPOT 2data (NIR band)
2
R = 0.4702
R = 0.6117
R2 = 0.4702
R2 = 0.6117
R2 = 0.7910
R2 = 0.7918
MODIS at 1 km resolution
MODIS at 250 m resolution
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12. First results
• Possible application: one-step radiometric
normalization of high-resolution imagery
by using same-day MODIS surface
reflectance.
• What next? How to handle ever-changing
observation geometries as a time series?
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56. Then, radiometric values are assigned to each
observation unit (parcel) for each MODIS overpass
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Calculation based on area-weigthed mean of retained pixels
70. Conclusions
• Gridding is a major source of inaccuracy and noise
• New polygon representation of MODIS observations has
significantly increased correlation with same-day highresolution data: better representation of observation
geometry
• Landscape objects delineated a priori can be efficiently
used to construct time series
• Data processing requires more computing power, but the
user has full control over the process (thresholds, quality
measures, etc.) and can obtain more accurate data with
maximal spatial and temporal coverage
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71. Outlook
• Currently: „proof of concept” level - further work
on real case studies needed
• Point Spread Function is another source of
inaccuracy – could be integrated
• Other data representations (Spline
surface, SensorML, etc.) are also to be
assessed
• Data processing speed is already good
(Python/PostgreSQL/PostGIS), but can be
further improved by e.g. parallel computing in
cloud architecture: implementation of IQmulus
project service
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72. Thank you!
Questions?
A High-volume Fusion and Analysis
Platform for Geospatial Point
Clouds, Coverages and Volumetric
Data Sets
Dániel Kristóf
kristof.daniel@fomi.hu
www.iqmulus.eu
IQmulus (FP7-ICT-2011-318787) is a 4-year Integrating Project (IP) in the
area of Intelligent Information Management within ICT 2011.4.4 Challenge
4: Technologies for Digital Content and Languages. IQmulus started on
November 1, 2012, and will finish October 31, 2016.
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