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Monday 11 June, 10:30 – 11:20 Lidar ground truth and applicaons (Brunt) Notes: The goal of this lecture is to cover applicaons of laser almetry. These include both absolute and relave applicaons, i.e., applicaons that require absolute accuracy of the measurement, such as height of the ice sheet, verses applicaons that use a differenal method, such as thickness of sea ice. This lecture will also cover validaon of almetry data, which is a precursor to the science applicaons discussed. ICESat-2 mission requirements: a) ICESat-2 shall produce an ice surface elevaon product that enables determinaon of ice-sheet elevaon change rates to an accuracy of beer than or equal to 0.4 cm/yr on an annual basis. b) ICESat-2 shall produce an ice surface elevaon product that enables determinaon of annual surface elevaon change rates on outlet glaciers to an accuracy of beer than or equal to 25 cm/yr over areas of 100 km 2 for year-to-year averages. c) ICESat-2 shall produce an ice surface elevaon product that enables determinaon of surface elevaon change rates for dynamic ice features that are intersected by its set of repeated ground-tracks to an accuracy of beer than or equal to 40 cm/yr along 1-km track segments. d) ICESat-2 shall produce an ice surface elevaon product that enables resoluon of winter (accumulaon) and summer (ablaon) ice-sheet elevaon change to 10 cm at 25-km x 25-km spaal scales. e) ICESat-2 shall provide monthly surface elevaon products to enable, when sea surface height references (leads) are available and under clear sky condions, the determinaon of sea-ice freeboard to an uncertainty of less than or equal to 3 cm along 25-km segments for the Arcc and Southern Oceans; the track spacing should be less than or equal to 35 km at 70 degrees latude on a monthly basis. Validaon methods 1) Crossover analysis -Relave sense of accuracy; -Assessment of precision or repeatability -Stascal based -Internal consistency 2) Direct comparison with ground-based data -Absolute sense of accuracy and precision -Bolivia: 50 by 50 km -Summit: 6 km along-track -88S Traverse: ~300 km, intersects 277 ICESat-2 RGTs

Monday 11 June, 10:30 – 11:20 Lidar ground truth and ... · Monday 11 June, 10:30 – 11:20 Lidar ground truth and applications (Brunt) Notes: The goal of this lecture is to cover

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Page 1: Monday 11 June, 10:30 – 11:20 Lidar ground truth and ... · Monday 11 June, 10:30 – 11:20 Lidar ground truth and applications (Brunt) Notes: The goal of this lecture is to cover

Monday 11 June, 10:30 – 11:20 Lidar ground truth and applications (Brunt)

Notes:The goal of this lecture is to cover applications of laser altimetry. These include both absolute and relative applications, i.e., applications that require absolute accuracy of the measurement, such as height of the ice sheet, verses applications that use a differential method, such as thickness of sea ice. This lecture will also cover validation of altimetry data, which is a precursor to the science applications discussed.

ICESat-2 mission requirements:

a) ICESat-2 shall produce an ice surface elevation product that enables determination of ice-sheet elevation change rates to an accuracy of better than or equal to 0.4 cm/yr on an annual basis.

b) ICESat-2 shall produce an ice surface elevation product that enables determination of annual surface elevation change rates on outlet glaciers to an accuracy of better than or equal to 25 cm/yr over areas of 100 km2 for year-to-year averages.

c) ICESat-2 shall produce an ice surface elevation product that enables determination of surface elevation change rates for dynamic ice features that are intersected by its set of repeated ground-tracks to an accuracy of better than or equal to 40 cm/yr along 1-km track segments.

d) ICESat-2 shall produce an ice surface elevation product that enables resolution of winter (accumulation) and summer (ablation) ice-sheet elevation change to 10 cm at 25-km x 25-km spatial scales.

e) ICESat-2 shall provide monthly surface elevation products to enable, when sea surface height references (leads) are available and under clear sky conditions, the determination of sea-ice freeboard to an uncertainty of less than or equal to 3 cm along 25-km segments for the Arctic and Southern Oceans; the track spacing should be less than or equal to 35 km at 70 degrees latitude on a monthly basis.

Validation methods

1) Crossover analysis-Relative sense of accuracy; -Assessment of precision or repeatability-Statistical based-Internal consistency

2) Direct comparison with ground-based data-Absolute sense of accuracy and precision-Bolivia: 50 by 50 km-Summit: 6 km along-track-88S Traverse: ~300 km, intersects 277 ICESat-2 RGTs

Page 2: Monday 11 June, 10:30 – 11:20 Lidar ground truth and ... · Monday 11 June, 10:30 – 11:20 Lidar ground truth and applications (Brunt) Notes: The goal of this lecture is to cover

Validation considerations:1) Target accuracy or precision2) Error on measurements (on ground-based or airborne data)3) Length and time scales represented in validation data(How representative is your dataset? How long will it be a meaningful validation dataset?)4) What terms bring your measurement back to the snow surface?

Applications requiring absolute accuracy:East Antarctic Ice Sheet requires sub-cm accuracy-Ice-sheet change

Applications based on differential methods:Less stringent accuracy requirements-Sea ice thickness-Subglacial lake identification-Subglacial lake interconnectivity-Grounding zone identification-Grounding zone sensitivities

Page 3: Monday 11 June, 10:30 – 11:20 Lidar ground truth and ... · Monday 11 June, 10:30 – 11:20 Lidar ground truth and applications (Brunt) Notes: The goal of this lecture is to cover

GPSPC = ~1000 mhNGSmodel = ~5 cmhAntHeight = ~150 – ~300 cmhTrackDepth = ~5 cm (Summit); ~10 cm (88S)