DEPARTMENT OF GEOMATIC ENGINEERING From 1m to the planet: mapping global population using Earth Observation: An Overview Jan-Peter Muller Professor of Image Understanding and Remote Sensing MODIS & MISR Science Team Member (NASA EOS Project) POLDER (ADEOSI/II), VEGETATION (SPOT4), GLI (ADEOSII) Workshop on Gridding Population Data Columbia University, New York Tuesday 2nd May 2000
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DEPARTMENT OF GEOMATIC ENGINEERING
From 1m to the planet: mapping global population using Earth Observation: An
Overview
Jan-Peter Muller
Professor of Image Understanding and Remote SensingMODIS & MISR Science Team Member (NASA EOS Project)
POLDER (ADEOSI/II), VEGETATION (SPOT4), GLI (ADEOSII)
Workshop on Gridding Population Data Columbia University, New York
Tuesday 2nd May 2000
DEPARTMENT OF GEOMATIC ENGINEERING
Overview How can we use remote sensing to measure what is of
relevance to global population mapping? Current Space Earth Observation platforms of relevance Exemplar 1: MODIS & VEGETATION for land surface
BRDF/albedo for mapping large-scale urban structures Exemplar 2: ERS SAR interferometry for mapping urban land
use and land use change at the sub-hectare scale Exemplar 3: IRS-1C for mapping urban land use for European
cities (EU MURBANDY) Exemplar 4: IKONOS-2 for automated building detection and
extraction (including height) Exemplar 5: POLDER & MISR for mapping aerosol sources Exemplar 6: MOPITT for mapping CO CEOS-IGOS Project proposal: Global mapping of urban
Very High resolution (≤5m IFoV)– IKONOS-2 (≥9/99 ->)
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How can we use remote sensing to measure what is of relevance to global
population mapping? Currently civilian remote sensing can not be used to identify the location of people so have to infer anthropogenic activity from….
Land cover, land use and land use changes (including 3D)– Traditional remote sensing techniques employ classification of single or
multiple (time series) of multi-spectral images» Problem is mixed signals from gardens & parks» Requires initial training sites to identify urban signals (very costly)
– SAR (Synthetic Aperture Radar) interferometry (IfSAR) has strong reflection from “hard targets” such as buildings, roads or railways. However, visibility of objects is illumination angle dependent. IfSAR v. good for fragmentation.
– BRDF/albedo related to land surface object geometry (e.g. urban, deforestation, desertification) and so exploit multi-angle RS signatures
– Night-time lights only visible where and when cloud cover is absent and where signal sufficiently strong to be detectable & difficult to interpret
– 3D elevations with very high resolution images can be used to extract automatically individual 3D built settlement locations
Anthropogenic activity - link to global change & human health
Urban areas well identified at 1km Extension to global unlikely due to
the high cost of the data
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Exemplar 1 : MODIS BRDF-derived Nadir reflectance & Albedo. Global maps at 1km being produced every 16 days
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Exemplar 2: Interferometric SAR for built environment area
mapping: The UK LANDMAP Project to create a DEM
and orthorectified LANDSAT, SPOT & ERS IfSAR Interferometric SAR excellent for
mapping of Built environment– Potential down to resolutions of 30m ~
0.3 hectares– Initial test over the British Isles as by-
product of the LANDMAP project– Potential to map settlements where
Night-light data is absent (developing world).
– Can be done daytime and/or night-time– Not dependent on cloud-free conditions
Urban areas are highly coherent especially over longer (inter-seasonal) temporal baselines
Development can be tracked on an annual (or even shorter) timescale
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Exemplar 2: False Colour composite and processed classified image of 3 band IfSAR data (Doll & Muller, ISPRS Congress 2000)
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DEPARTMENT OF GEOMATIC ENGINEERING
Exemplar 3: EU MURBANDY - application of traditional photo-interpretation to urban land use classification using IRS-1C for Vienna, AU.
20 EU cities selected for pilot project. http://murbandy.sai.jrc.it/
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Exemplar 4: DSEM (Digital Surface Elevation Model) from simulated 1m spaceborne stereo-optical sensors with digital map data superimposed. Such DSEMs can
be used to extract single buildings
St Albans, UK≤30m AGL (Red)≈ AGL (Green)≤-3m AGL (Blue
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Exemplar 4: IKONOS-2 off-nadir 79cm image over the
Exemplar 5: Aerosol Mapping and Monitoring from POLDER @6.7km -
example of DAILY air pollution (PM) maps over Mexico city
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Example 5: MISR imaging geometry - multi-angular sampling for surface BRDF, aerosol retrieval and stereo
Cloud-top heights & winds
9 pushbroom cameras4 spectral bands275m off-nadir,250m nadir IFoVSwath≈380kmRepeat time ≈3-9 days
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Example of MISR 3-band multi-look (all 9 angles) imagery
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Example MISR nadir vs 70ºf view of aerosols
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Examplar 6: Examples of anthropogenic and natural urban-atmosphere interactions from MODIS, CERES &
MOPITT
QuickTime™ and aCinepak decompressor
are needed to see this picture.
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CEOS-IGOS Project proposal: Global mapping of urban population
At a recent CEOS (Committee on Earth Observing Systems) WGISS (Working Group on Information Systems) meeting held at UCL, UK it was suggested that a new IGOS (International Global Observing System) project should be initiated along the lines of either the global Carbon Inventory or the global Forest Map project. This idea is currently being debated by email.
IGOS are prototype very large-scale projects with active support from the space agencies who provide not only data but often funding for the generation of value-added products. It is not restricted to the academic community but includes government and the private sector
Given the results of this workshop (and especially this session), should we push within CEOS to establish this project?
Is there sufficient scientific justification even given the uncertainties?