Global Inventory of Human Settlements
Derived From DMSP-OLS Data
Christopher Elvidge
Solar-Terrestrial Physics Division
NOAA National Geophysical Data Center
325 Broadway, Boulder, Colorado 80303 USA
Tel. 303-497-6121 Fax: 303-497-6513
E-mail:cde@ngdc.noaa.gov
Yoshiaki Honda
Center for Environmental Remote Sensing
Chiba University
1-33 Yayoi-cho,Inage-ku, Chiba 263 japan
Tel. 81-43-290-3835 Fax: 81-43-290-3857
E-mail:yhonda@rsic.cr.chiba-u.ac.jp
Abstract
The first 1 km resolution global inventory of human settlements is near completion. The product is being assembled using a 1994-95 time series of nighttime visible band observations from the Defense Meteorological Satellite Program (DMSP) Operational Linescan System (OLS). Preliminary results indicate that area lit is highly correlated to measures of economic activity, such as Gross Domestic Product (GDP)
Introduction
Much of global change research is dedicated to discerning and documenting the impacts of human activities on natural systems. Human population numbers have expanded from ~750 million in the mid-1700's to 5.8 billion in 1996 and are expected to double in the next 45 years. Human activities which are known to be cumulatively altering the global environment include greenhouse gas emissions from fossil fuel consumption, air and water pollution, and land cover/ land use change. Far from being evenly distributed across the land surface, to a great extent human activities with environmental consequences are concentrated in the vicinity of human population centers. As a contribution to global environmental research, we are producing a satellite data derived map of human settlements at 1 km resolution.
Materials and Methods
The DMSP-OLS has a unique capability for the global observation of fires and human settlements. The primary function of the DMSP-OLS is to provide global imagery of cloud cover. At night the observed visible near infrared (VNIR) radiance is intensified, for the purpose of cloud detection using moonlight. In addition to moonlit clouds, the light intensification makes it possible to detect VINIR emissions emanating from the earth's surface, from cities, towns, industrial sites, gas flares, and ephemeral events such as fires and lightning. NDGC serves as the nation's long term archive for DMSP data. NGDC currenly receives 7.4 gigabytes of raw DMSP data per days using a dedicated T-1 line to the U.S. Air Force, Offutt Air Base, Omaha, Nebraska. Data transfers occur automatically, as readouts are received by Offutt, and arrive on the NGDC computer within 1-2 hours from the observation time (longest delay comes from the time gaps between successive readouts of the on-board tape recorders). At NGDC the data are deinterleaved and written out to archive tapes. Our near-real-time global DMSP data stream, ingest, preprocessing, and product generation are analogs for EOS-MODIS. It is anticipated that the DMSP -OLS data stream will continue to flow to NGDC until 2010 or anticipated that the DMSP-OLS data stream will continue to flow to NGDC until 2010 or even 2015. The nighttime low light imaging capabilities of the OLS will be continued even 2015. The nighttime low light imaging capabilities of the OLS will be continued in the combined DoD -NOAA polar orbiting meteorological satellite program (NPOES).
We have developed algorithms for mapping fires, human settlements, and gas flares using time series of nighttime DMSP-OLS observations (Elvidge et al., 1997a). NGDC is currently completing the first systematic global inventory of human settlements based on satellite observations. NGDC has completed a five year (1992-96) nightly inventory of fires in Madagascar for the U.S. AID using DMSP-OLS data. The core set of algorithms and details regarding the sensor and data characteristics are described in Elvidge et al. (1997a). This reference can be viewed at the "Nighttime Lights of the World" (http://WWW.ngdc.noaa.gov: 8080/production/html/BIOMAS/night.html). NGDC is completing a global inventory of stable lights using a times series of nighttime OLS observations from 1994-95. Imagery are only used from the dark half of each lunar cycle to avoid problems with moonlight clouds and moonlight reflections of water bodies.
