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Deriving a climate temperature record from satellite data
Data from the Geostationary Operational Environmental Satellite series is analyzed to yield information about land surface temperature.
23 June 2009, SPIE Newsroom. DOI: 10.1117/2.1200906.1637
Temperatures at the Earth's surface are important for the study of global warming. Typically, global temperature change is assessed by in situ surface air temperature (SAT) measurements at 2m height at weather stations. The diurnal temperature range (DTR) is also an important index of climate change.1–5 Until recently, most information on DTR also came from SATs, based on station observations. Strong diurnal and seasonal cycles are identified in SAT.6,7 However, weather stations are usually located in relatively densely populated regions where anthropogenic impacts may affect measurements, and thus the temperature record may not be representative of global change. Moreover, station observations are sparse and unevenly distributed, and they suffer from differences in elevation and time of observation.8 The use of satellite-derived data could contribute to a globally consistent measurement.9
Most surface temperature retrievals from satellites are based on polar orbiters.10–15 Surface temperature, especially land surface temperature (LST), has a strong diurnal cycle, which cannot be captured at the temporal resolution (approximately two views per day) of such satellites. Only two points in the cycle are measured, and the sampling is neither continuous nor homogeneous because the exact timing of these two points will drift. The drift in local equatorial crossing time of the US National Oceanic and Atmospheric Association (NOAA) series of polar-orbiting satellites,16 for example, leads to a non-climatic trend in surface temperature, which degrades the usefulness of LST measurements from those satellites. Geostationary satellites, on the other hand, provide good diurnal coverage, making them attractive for deriving information on the diurnal LST cycle.17–19
Figure 1. The GOES-8 (red) and GOES-12 (green) bands.
One of our current projects is to derive long-term climate surface temperature records from the NOAA Geostationary Operational Environmental Satellite (GOES) series. In addition to problems with maintaining consistent calibration over time, changes in GOES imager channels are also a big concern. GOES-8 has the traditional split-window channels that can be used for atmospheric correction. We have worked extensively with algorithm development and surface temperature retrieval from GOES-8, and its surface skin temperature algorithm is relatively mature. However, the GOES M (12) through Q series satellites lack the split-window channels that would enable the evaluation of LST based on differential atmospheric (water vapor) absorption in two infrared channels.18 (Figure 1 compares the GOES-8 and GOES-12 bands.) Therefore, I proposed a two-channel algorithm using the characteristics of the mid-infrared channel (3.9μm) with less atmospheric absorption, and one channel (11μm) plus a water-vapor correction algorithm. Using this algorithm, surface temperature can be derived from the current GOES-M and GOES-Q data, as shown in Figure 2.
The evaluation of surface temperature retrievals from satellites has been difficult, since satellites measure skin temperature at the pixel level, while global-scale ground observations are from shelters at point scale. Due to the lack of ground observations,17,18 I attempted to use various available surface observations, directly and indirectly related to surface skin temperature, including atmospheric radiation measurement, Surface Radiation Network data, and Mesonet observations, to evaluate LST values retrieved from GOES satellites. These evaluations indicate that the results shown in Figure 2 provide a reasonably accurate record of surface temperature.
My colleagues and I are in the process of generating a consistent surface temperature record from the GOES series satellites.
Figure 2. LST derived from the GOES-12 observations.
George Mason University
College of Science, Geography and Geoinformation Science Department
2. T. R. Karl, P. D. Jones, R. W. Knight, G. Kukla, N. Plummer, V. Razuvayev, K. P. Gallo, J. Lindseay, R. J. Charlson, T. C. Peterson, A new perspective on recent global warming, Bull. Am. Meteorol. Soc. 74, pp. 1007-1023, 1993.
5. Intergovernmental Panel on Climate Change in Climate Change, J. T. Houghton, Y. Ding, D. J. Griggs, M. Noguer, P. J. van der Linden, X. Dai, K. Maskell, and C. A. Johnson (eds.), The Scientific Basis, Cambridge Univ. Press, Cambridge, U.K., 2001.
16. A. Ignatov, I. Laszlo, E. D. Harrod, K. B. Kidwell, G. P. Goodrum, Equator crossing times for NOAA, ERS and EOS sun synchronous satellites, Int'l J. Remote Sens. 25, no. 23, pp. 5255-5266, 2004.