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NASA/TM--2000-209891, Vol. 58 Technical Report Series on the Boreal Ecosystem-Atmosphere Study (BOREAS) Forrest G. Hall and Jaime Nickeson, Editors Volume 58 BOREAS RSS-11 Ground Network of Sunphotometer Measurements B.L. Markham and J. Schafer National Aeronautics and Space Administration Goddard Space Flight Center Greenbelt, Maryland 20771 August 2000 The NASA STI Program Office ... in Profile Since its founding, NASA has been dedicated to • CONFERENCE PUBLICATION. Collected the advancement of aeronautics and space papers from scientific and technical science. The NASA Scientific and Technical conferences, symposia, seminars, or other Information (STI) Program Office plays a key meetings sponsored or cosponsored by NASA. part in helping NASA maintain this important role. • SPECIAL PUBLICATION. 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Hall and Jaime Nickeson, Editors Volume 58 BOREAS RSS-11 Ground Network of Sunphotometer Measurements Brian L. Markham, Goddard Space Flight Center, Greenbelt, Maryland Joel Schafer, Raytheon ITSS National Aeronautics and Space Administration Goddard Space Flight Center Greenbelt, Maryland 20771 August 2000 Available from: NASA Center for AeroSpace Information National Technical Information Service 7121 Standard Drive 5285 Port Royal Road Hanover, MD 21076-1320 Springfield, VA 22161 Price Code: AI7 Price Code: AI0 BOREAS RSS-11 Ground Network of Sunphotometer Measurements Brian L. Markham, Joel Schafer Summary The BOREAS RSS-11 team operated a network of five automated (Cimel) and two hand-held (Miami) solar radiometers from 1994 to 1996 during the BOREAS field campaigns. The data provide aerosol optical depth measurements, size distribution, phase function, and column water vapor amounts over points in northern Saskatchewan and Manitoba, Canada. The data are useful for the correction of remotely sensed aircraft and satellite images. The data are provided in tabular ASCII files. Table of Contents 1) Data Set Overview 2) Investigator(s) 3) Theory of Measurements 4) Equipment 5) Data Acquisition Methods 6) Observations 7) Data Description 8) Data Organization 9) Data Manipulations 10) Errors 11) Notes 12) Application of the Data Set 13) Future Modifications and Plans 14) Software 15) Data Access 16) Output Products and Availability 17) References 18) Glossary of Terms 19) List of Acronyms 20) Document Information 1. Data Set Overview 1.1 Data Set Identification BOREAS RSS- 11 Ground Network of Sunphotometer Measurements 1.2 Data Set Introduction A ground-based sunphotometer network was installed within the BOReal Ecosystem-Atmosphere Study (BOREAS) study areas to characterize the size and distribution of atmospheric aerosols and column water vapor amount and to aid in the correction of aircraft and satellite imagery. Automated sunphotometer data are available fairly continuously from early 1994 through 1996 for two sites in the Northern Study Area (NSA) and two in the Southern Study Area (SSA). Data were collected from a fifth automated instrument located at the Flin Flon airport at the Manitoba/Saskatchewan border; this instrument was moved in 1996 to Paddockwood, SK, in the SSA. Measurements made by two additional hand-held instruments, operated during the 1994-96 time period at each of the study areas, are also a part of this data set. A local observer made the hand-held measurements near noon when the Sun was not obscured by any clouds. Page 1 1.3 Objective/Purpose The purpose was to establish a data set of aerosol, water vapor, and ozone atmospheric properties in the BOREAS region for a 3-year period for use by BOREAS in atmospheric correction of remotely sensed data. Another goal was to establish an aerosol climatology of the region by specifying, for example, the annual cycle of aerosol loading across the region. 1.4 Summary of Parameters Parameters: Direct solar irradiance (340, 380, 440, 500, 670, 870, 1020 nm) Sky radiance (440, 670, 870, 1020 nm) Aerosol optical thickness Column water vapor amount 1.5 Discussion A network of five automated (Cimel) and two hand-held (Miami) solar radiometers were operated during the 1994-96 time period for BOREAS to provide aerosol optical depth measurements, size distribution, phase function, and column water vapor amounts. The purpose was to establish a data set of aerosol, water vapor, and ozone atmospheric properties in the BOREAS region for a 3-year period for use by BOREAS in atmospheric correction of remotely sensed data. 1.6 Related Data Sets BOREAS RSS-03 Reflectance Measured from a Helicopter-Mounted Barnes MMR BOREAS RSS-12 Airborne Tracking Sunphotometer Measurements BOREAS RSS-12 Automated Ground Sun Photometer Measurements in the SSA BOREAS RSS-18 Ground Sunphotometer Measurements in the SSA An additional data set collected and used in comparison was sunphotometer measurements made by Norman O'Neill (RSS-19) at the Canada Centre for Remote Sensing (CCRS). These data were not submitted to the BOREAS Information System (BORIS). 2. Investigator(s) 2.1 Investigator(s) Name and Title Brian L. Markham Physical Scientist 2.2 Title of Investigation Characterization of Atmospheric Optical Properties for BOREAS 2.3 Contact Information ContaCt 1: Brian L. Markham NASA GSFC Code 923 Greenbelt, MD 20771 (301) 614-6608 (301) 614-6695 (fax) Brian.L.Markham. [email protected] Page 2 Contact 2: JoelSchafer NASA GSFC Code923 Green.belt,MD 20771 (301)614-6668 (301)614-6695(fax) [email protected] Contact 3: JaimeNickeson RaytheonITSS NASA GSFC Code923 Greenbelt,MD 20771 (301)286-3373 (301)286-0239(fax) [email protected] 3. Theory of Measurements Sunphotometers measure direct surface irradiance. Because direct solar irradiance depends on the atmospheric transmission, the components affecting this transmission such as aerosol optical thickness (AOT), water vapor column abundance, ozone absorption, and molecular scattering can either be estimated or bemeasured. Optical thickness is calculated from spectral extinction of direct beam radiation at each wavelength based on Beer's Law: where: VK = digital voltage measured at wavelength k V o - R 2 • e Vo= extraterrestrial voltage m = optical airmass 12= total optical thickness R = relative Earth-Sun distance Attenuation due to Rayleigh scatter, and absorption by ozone and gaseous pollutants is estimated and removed to isolate the AOT (12). The dependence of transmission, Tw, on water column abundance can be written as the following [Halthore et al., 1992, Bruegge et al, 1992]: W = vertical column abundance (cm) -a-m b .wb where: a, b = constants that depend on the wavelength T =e position, width and shape of the filter function, and atmospheric conditions. Sky radiance measurements are inverted with radiative transfer equations lNakajima et al., 1983] to provide aerosol properties of size distribution and phase function over the particle size range of 0.1 to 5 jam. Page 3 4. Equipment 4.1 Sensor/Instrument Description 4.1.1 Collection Environment The automated sunphotometers operated during nonwinter months according to their diurnal schedule (Section 4.1) when there was no precipitation and the atmosphere is clear enough to allow the instrument to focus on

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