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T066% -368 F 2060 2 t066% -368 f 2060_2 ANALYSIS OF AIRBORNE RADAR ALTIMETRY MEASUREMENTS OF THE GREENLAND ICE SHEET A Dissertation Presented by ELLEN J. FERRARO Submitted to the Graduate School of the University of Massachusetts Amherst in partial fulfillment of the requirements for the degree of DOCTOR OF PHILOSOPHY May 1994 Department of Electrical and Computer Engineering (_) Copyright Ellen J. Ferraro 1994 All Bights Reserved ANALYSIS OF AIRBORNE RADAR ALTIMETRY MEASUREMENTS OF THE GREENLAND ICE SHEET A DissertationPresented by ELLEN J. FERRARO A_content by: Calvin T. Swift,Chair Robert E. McIntosh, Member. Patrick A. Kelly, Member (_/ J_gham_.grctte, Member • ver, Department Head . Electrical& Computer Engineering To Morn and Dad ACKNOWLEDGMENTS During my graduate school years, I have had the invaluable opportunity to not only study microwave remote sensing of the earth, but also to design and manage a project from its development through to its final stages of experiment and data analysis. As my advisor, Dr. CMvin T. Swift allowed me to make my own decisions as well as make my own mistakes, while providing the guidance and encouragement necessary as I progressed from a shy and naive first year graduate student to a doctoral recipient. I would like to thank him for this guidance and for the opportunity to travel to unique places such as Greenland, Iceland and Newfoundland. Both Dr. Calvin T. Swift and Dr. Robert E. Mclntosh deserve thanks for providing the exce]]ent facilities and equipment available in the Microwave Remote Sensing Laboratory, without which none of this work would have been possible. I would also like to thank Dr. Patrick Kelly for serving on my committee and Dr. Julie Brigham-Grette for her help in preparing for my trip to Greenland and for serving on my committee. When the design for the refurbished AAFE altimeter was first being developed, Dr. Chris Rapley, Dr. Seymour Laxon and many other scientists at the Mullard Space Science Laboratory provided invaluable suggestions on current tracking tech- niques and problems with previous tracking methods, as we]] as a tremendous amount of literature on radar altimetry. Once the AAFE system was completely developed I spent numerous hours at the NASA Wallops Flight Facility installing and testing the instrument. I would like to thank the aircraft crew and pilots at Wallops for their assistance and friendship. In addition I would like to thank the Observational Sciences Branch_ especially Bill Krabil] and Earl Frederick for their V patience and help in providing GPS, AOL and INS data and for their friendship. Everyone at Wallops knew how to make a Yankee feel welcome and comfortable on the eastern shore of Virginia. During my last summer in MIRSL, I spent four weeks on the Greenland ice cap. Despite inhibitions about camping on an ice sheet without heat or hot water, it turned out to be a fun and adventure-some experience, primarily due to the help and friendship of Ingrid Zabel, Paul Baggeroer, Henry Brecher, Mark Anderson and Clint Rowe. I would especially like to thank Clint Rowe and Mark Anderson for their help in the probing experiment. I would also like to thank Dr. Robert Thomas for providing the funding for this project under NASA grant NCT-50606, Matthew Grund for operating the AAFE altimeter during the 1993 experiment, Wayne Boncyk for his help in developing the data acquisition system of the radar and the numerous other past and present MIRSL graduate students whose suggestions, help and friendship aided in the devel- opment of this project. In addition, I would like to thank Claire Hopley for reading and editing this dissertation. There are many people who helped me through the difficult times in both undergraduate and graduate school, but the person that deserves the most thanks is Dean Nancy HeUman for her encouragement, guidance and friendship. Finally, I would like to thank my friends and family, especially my parents Neal and Bernice Martin, for their love and support throughout the past twenty-six years. I love all of you and none of this would have been worth while if it were not for the opportunities to go home and share these experiences with you. Above all, I thank my husband and friend for life, Paul Ferraro, for his love, his support and for the lifetime that we will share together. vi ABSTRACT ANALYSIS OF AIRBORNE RADAR ALTIMETRY MEASUREMENTS OF THE GREENLAND ICE SHEET MAY 1994 ELLEN J. FERRARO B.S.E.E., UNIVERSITY OF MASSACHUSETTS AMHERST PH.D._ UNIVERSITY OF MASSACHUSETTS AMHERST Directed by: Professor Calvin T. Swift This dissertation presents an analysis of airborne altimetry measurements taken over the Greenland ice sheet with the 13.9 GHz Advanced Apphcation Fhght Ex- periment (AAFE) pulse compression radar altimeter. This Ku-band instrument was refurbished in 1990 by the Microwave Remote Sensing Laboratory at the University of Massachusetts to obtain high-resolution altitude measurements and to improve the tracking, speed, storage and display capabilities of the radar. In 1991 and 1993, the AAFE altimeter took part in the NASA Multisensor Airborne Altimetry Experiments over Greenland, along with two NASA laser altimeters. Altitude results from both experiments are presented along with comparisons to the laser altimeter and calibration passes over the SondrestrSm runway in Greenland. Although it is too early to make a conclusion about the growth or decay of the ice sheet, these results show that the instrument is capable of measuring small-scale surface changes to within 14 centimeters. In addition, results from these experiments reveal that the radar is sensitive to the different diagenetic regions of the ice sheet. Return waveforms from the wet- snow, percolation and dry-snow zones show varying effects of both surface scattering and sub-surface or volume scattering. Models of each of the diagenetic regions of Greenland are presented along with parameters such as rms surface roughness, rms vii surface slopeand attenuation coetTicient of the snow pack obtained by fitting the models to actual return waveforms. °oo Vlll TABLE OF CONTENTS P _st ACKNOWLEDGMENTS ........................................ v ABSTRACT ................................................ vii LIST OF TABLES ........................................... xi LIST OF FIGURES ........................................... xii CHAPTERS I. INTRODUCTION ........................................... 1 i.I History of Radar Altimetry ....................... 1 1.2 Scientific Motivation ........................... 2 1.3 Summary of Chapters .......................... 4 2. PRINCIPLES OF RADAR ALTIMETRY ........................... 6 2.1 Altitude Measurements ......................... 6 2.2 Pulse compression ............................ 8 2.3 Mode of Operation ........................... 16 3. AAFE RADAR ALTIMETER SYSTEM ........................... 24 3.1 Radar System Hardware ........................ 25 3.1.1 Transmitter Subsystem ..................... 28 3.1.2 Antenna ............................. 31 3.1.3 Receiver Subsystem ....................... 31 3.1.4 Data Acquisition Subsystem .................. 36 3.1.5 Tracking Subsystem ....................... 40 3.1.6 Control Subsystem ....................... 47 3.2 System Calibration ........................... 49 3.2.1 Internal Calibration ....................... 49 3.2.2 External Calibration ....................... 55 3.3 Noise Analysis .............................. 55 3.3.1 System Signal-To-Noise Ratio ................. 55 3.3.2 Range Resolution ........................ 66 3.3.3 Quantization Noise ....................... 69 3.3.4 FFT Errors ............................ 69 ix 4. ALTIMETRYMEASUREMENTSOF THE GREENLAND ICE SHEET ........ 71 4.1 1991 Greenland Experiment ...................... 71 4.1.1 Experiment Description and Fhght Lines ........... 71 4.1.2 Runway Ground Truth Comparison .............. 72 4.1.3 Comparison with the AOL Laser Altimeter .......... 78 4.1.4 Comparison of Flight Line Cross-over Points ......... 88 4.1.5 Altitude Results ......................... 90 4.2 1993 Greenland Experiment ...................... 93 4.2.1 Experiment Description and Fhght Lines ........... 93 4.2.2 Runway Ground Truth Comparison .............. 98 4.2.3 Altitude Results ......................... 98 4.3 Comparison of 1991 and 1993 Elevation Measurements ........ 101 5. ANALYSIS OF WAVEFORMS FROM THE GREENLAND ICE SHEET ....... 106 5.1 Scattering Models of the Diagenetic Zones of Greenland ....... 110 5.1.1 Wet-snow Zone Model ...................... 110 5.1.2 Percolation Zone Model ..................... 120 5.1.3 Dry-snow Zone Model ...................... 132 5.2 Mapping Diagenetic Zones ....................... 144 5.3 Comparison of Retracking Algorithms ................. 148 6. CONCLUSIONS AND RECOMMENDATIONS FOR FUTURE RESEARCH ..... 159 REFERENCES .............................................. 161 X LIST OF TABLES Table Page 3.1 Table of AAFE parameters used to calculate the system signal-to- noise ratio .................................. 64 5.1 Table of the five parameters used in the least-mean-squared error fit to the surface scattering model ...................... 115 5.2 Table of the seven parameters used in the LMSE fit to the combined surface and Rayleigh volume scattering model .............. 140 5.3 Table of the five parameters used in the least-mean-squared error fit to the Martin et al. model ......................... 151 xi LIST OF FIGURES Figure Page 2.1 Principle of a radar altimeter altitude measurement ........... 7 2.2 Example of a
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