Timothy James Urban

Calibration and Verification of Jason-1 Using Global Along-Track Residuals with TOPEX

It is demonstrated that the Jason-1 measurements of sea surface height (SSH), wet path delay, and ionosphere path delay are within required accuracies, via a global cross-calibration with similar measurements made by TOPEX/Poseidon (T/P) over a 6-month period. Since the two satellites were on the same groundtrack separated in time by only 70 s, measurements were recorded at approximately the same location and time. The variations in the wet path delay measured by Jason-1 compared to T/P are only 5 mm RMS, well within the required performance of 1.2 cm RMS. The RMS of the ionosphere differences is also well within the expected values, with a mean RMS of 1.2 cm. The largest difference is that the Jason-1 SSH is biased high relative to T/P SSH by 144 mm after the T/P and Jason-1 data are both corrected with improved sea state bias (SSB) models. However, the bias will change if a different SSB model is used, so the user should be cautious that the bias used matches the SSB models. The bias is generally constant within ± 10 mm in the open ocean, but appears to be higher or lower in some regions. Additionally, the SSH has been verified by comparison with 36 island tide gauges over the same period. After removing the global relative bias, the Jason-1 SSH data agree with tide gauges within 3.7 cm RMS and with T/P data within about 3.5 cm RMS on average for 1-s measurements, meeting the required accuracy of 4.2 cm RMS.

ICESat Altimetry Data Product Verification at White Sands Space Harbor

Three unique techniques have been developed to validate the Ice, Cloud, and Land Elevation Satellite (ICESat) mission altimetry data product and implemented at White Sands Space Harbor (WSSH) in New Mexico. One specific technique at WSSH utilizes zenith-pointed sensors to detect the laser on the surface and enable geolocation determination of the altimeter footprint that is independent of the data product generation. The system of detectors also registers the laser light time of arrival, which is related to the data product time tag. Several overflights of the WSSH have validated these time tags to less than 3plusmn1 mus. The ground-based detector system also verified the laser illuminated spot geolocation to 10.6 m (3.5 arcsec) plusmn4.5 m on one occasion, which is consistent with the requirement of 3.5 m (1sigma). A third technique using corner cube retroreflector signatures in the altimeter echo waveforms was also shown to provide an assessment of the laser spot geolocation. Although the accuracy of this technique is not equal to the other methodologies, it does offer position determination for comparison to the spacecraft altimetry data product. In addition, elevation verifications were made using the comparison of the ICESat elevation products at WSSH to those acquired with an airborne light detection and ranging. The elevation comparisons show an agreement to within plusmn34 cm (plusmn6.7 cm under best conditions) which indicate no significant errors associated with the pointing knowledge of the altimeter

Calibration and Verification of Jason-1 Using Global Along-Track Residuals with TOPEX Special Issue: Jason-1 Calibration/Validation

It is demonstrated that the Jason-1 measurements of sea surface height (SSH), wet path delay, and ionosphere path delay are within required accuracies, via a global cross-calibration with similar measurements made by TOPEX/Poseidon (T/P) over a 6-month period. Since the two satellites were on the same groundtrack separated in time by only 70 s, measurements were recorded at approximately the same location and time. The variations in the wet path delay measured by Jason-1 compared to T/P are only 5 mm RMS, well within the required performance of 1.2 cm RMS. The RMS of the ionosphere differences is also well within the expected values, with a mean RMS of 1.2 cm. The largest difference is that the Jason-1 SSH is biased high relative to T/P SSH by 144 mm after the T/P and Jason-1 data are both corrected with improved sea state bias (SSB) models. However, the bias will change if a different SSB model is used, so the user should be cautious that the bias used matches the SSB models. The bias is generally constant within ± 10 mm in the open ocean, but appears to be higher or lower in some regions. Additionally, the SSH has been verified by comparison with 36 island tide gauges over the same period. After removing the global relative bias, the Jason-1 SSH data agree with tide gauges within 3.7 cm RMS and with T/P data within about 3.5 cm RMS on average for 1-s measurements, meeting the required accuracy of 4.2 cm RMS.

Evaluation of GRACE and ICESat Mass Change Estimates Over Antarctica

The goal of this study is to examine some of the many corrections and processing strategies that can have a significant influence on the ice mass change estimates computed from GRACE and ICESat mission data. These two missions, when combined, have the potential to generate new insights into the mass balance and geophysical processes of regions such as Antarctica, where such quantities are currently not well understood. Key to this combination is the identification of the major sources of uncertainty in the data processing. For the ICESat data, this includes an analysis into the calculation of the campaign biases, assumptions regarding the firn density, and a comparison between height rates derived from crossover and repeat track analysis. For the GRACE data, the focus will be on the impact of various GIA models and other a priori input values (i.e., C 20, geocenter motion, etc.). Comparisons with the latest data releases for both missions will be presented for the 4 year period spanning from October 2003 to October 2007. Recommendations for future work will also be discussed.

Comparison of Small-footprint and Large-footprint Waveform Lidar for Terrestrial Surface Characterization

Small-footprint airborne lidar (Light Detection and Ranging) topographic mapping is widely used in the commercial and research sectors for applications including shoreline monitoring, forestry, flood zone delineation, and urban mapping. A new module developed by Optech, Inc. to digitally record the entire returned lidar pulse has been integrated into, and runs simultaneously with, a conventional small-footprint lidar system operated by the University of Texas (1). Small-footprint airborne waveform lidar data was flown over Freeman Ranch located in Central Texas on August 12, 2005. The objectives for the Freeman Ranch lidar project include 1) the comparison of waveform ranging to the standard discrete return Airborne Laser Terrain Mapping (ALTM) product and 2) the comparison of small-footprint waveform lidar to large-footprint waveform lidar from the Geoscience Laser Altimeter System (GLAS) onboard ICESat. The preliminary analysis of small-footprint waveforms indicates an overall improvement in canopy penetration and subsequent detection of underlying topography compared with the discrete ALTM last return. For the Freeman Ranch site, the small-footprint waveform data were synthesized to simulate a GLAS waveform using the same energy power distribution function as GLAS. Results indicate that synthesized waveforms were a good qualitative fit to the returned GLAS waveforms. However, preliminary analysis indicates an increase of error in the GLAS elevation with increasing amounts of woody cover within the footprint.

Use of Orbital LIDAR in the Brazilian Cerrado Biome: Potential Applications and Data Availability

This paper focuses on the Ice, Cloud and land Elevation Satellite (ICESat) Geoscience Laser Altimeter System (GLAS) data availability over the 2 million km2 Cerrado, the Brazilian central savanna biome and one of the world’s biodiversity hotspots. Overall, about 2.5 million laser shots, distributed along the seven years of ICESat operation (2003–2009) and comprising three major seasonal domains, were acquired, from which, 206,026 and 176,035 screened footprints are coincident with the remnant vegetation and cultivated pasture areas (the dominant land-use form in the Cerrado). Although these points are well distributed over the entire Cerrado, the ICESat track data collection results in substantial data gaps. In relation to the 15,612 Cerrado watersheds (6th order Otto basin system), 8,369 and 4,415 watersheds are completely deprived of data points over their remnant vegetation and pasture covers, respectively. Light Detection and Ranging (LIDAR) availability was also evaluated in relation to specific targets of interest, including both fully-protected conservation units as well as areas impacted by fire and deforestation. In spite of the very few occurrences, our assessments indicate that enough LIDAR data is available for retrieving structural and functional properties of a variety of Cerrado physiognomies, as well as to assess how these physiognomies respond to anthropogenic induced changes. In fact, the comprehensive data availability analysis conducted in this study corroborate the potential of GLAS LIDAR waveforms for the retrieval of biophysical properties at both local and regional scales, particularly concerning remnant carbon stocks and pasture conditions, key information for the conservation of the fast-changing and severely threatened Cerrado.