Gordon Ariho | University of Kansas (original) (raw)
Uploads
Papers by Gordon Ariho
Nature Geoscience, Oct 11, 2023
2022 IEEE International Symposium on Phased Array Systems & Technology (PAST)
IGARSS 2020 - 2020 IEEE International Geoscience and Remote Sensing Symposium, 2020
Differential Interferometric Synthetic Aperture Radar (DIn-SAR) processing techniques applied to ... more Differential Interferometric Synthetic Aperture Radar (DIn-SAR) processing techniques applied to ice penetrating radar enable precise measurement of the vertical displacement of englacial layers within an ice sheet. This technique has primarily been applied using ground based ice-penetrating radar due to the ability to achieve a near-zero spatial baseline. We investigate this technique on data from the Multichannel Coherent Radar Depth Sounder (MCoRDS), an airborne ice penetrating radar, and produce initial results from a high accumulation region near Camp Century in northwest Greenland. We estimate the vertical displacement by compensating for the spatial baseline using precise trajectory information and estimates of the cross-track layer slope from direction of arrival analysis. The measurement accuracy is still being investigated.
Nature Geoscience, Oct 11, 2023
2022 IEEE International Symposium on Phased Array Systems & Technology (PAST)
IGARSS 2020 - 2020 IEEE International Geoscience and Remote Sensing Symposium, 2020
Differential Interferometric Synthetic Aperture Radar (DIn-SAR) processing techniques applied to ... more Differential Interferometric Synthetic Aperture Radar (DIn-SAR) processing techniques applied to ice penetrating radar enable precise measurement of the vertical displacement of englacial layers within an ice sheet. This technique has primarily been applied using ground based ice-penetrating radar due to the ability to achieve a near-zero spatial baseline. We investigate this technique on data from the Multichannel Coherent Radar Depth Sounder (MCoRDS), an airborne ice penetrating radar, and produce initial results from a high accumulation region near Camp Century in northwest Greenland. We estimate the vertical displacement by compensating for the spatial baseline using precise trajectory information and estimates of the cross-track layer slope from direction of arrival analysis. The measurement accuracy is still being investigated.