open access publication

Article, 2024

The apparent effect of orbital drift on time series of MODIS MOD10A1 albedo on the Greenland ice sheet

Science of Remote Sensing, ISSN 2666-0172, Volume 9, Page 100116, 10.1016/j.srs.2023.100116

Contributors

Feng, Shunan 0000-0002-8534-3066 (Corresponding author) [1] Wehrlé, Adrien 0000-0002-4870-1821 [2] Cook, Joseph Mitchell 0000-0002-9270-363X [1] Anesio, Alexandre Magno 0000-0003-2990-4014 [1] Box, Jason Eric 0000-0003-0052-8705 [3] [4] Benning, Liane G 0000-0001-9972-5578 [5] [6] Tranter, Martyn 0000-0003-2071-3094 (Corresponding author) [1]

Affiliations

  1. [1] Aarhus University
  2. [NORA names: AU Aarhus University; University; Denmark; Europe, EU; Nordic; OECD];
  3. [2] University of Zurich
  4. [NORA names: Switzerland; Europe, Non-EU; OECD];
  5. [3] Geological Survey of Denmark and Greenland
  6. [NORA names: GEUS Geological Survey of Denmark and Greenland; Governmental Institutions; Denmark; Europe, EU; Nordic; OECD];
  7. [4] Geological Survey of Denmark and Greenland, Copenhagen, Denmark
  8. [NORA names: GEUS Geological Survey of Denmark and Greenland; Governmental Institutions; Denmark; Europe, EU; Nordic; OECD];
  9. [5] Freie Universität Berlin
  10. [NORA names: Germany; Europe, EU; OECD];

Abstract

The NASA MODIS MOD10A1 snow albedo product has enabled numerous glaciological applications. The temporal consistency of MODIS albedo is critical to obtaining reliable results from this 22-year time series. The orbit of Terra began to drift toward earlier acquisition times after the final inclination adjustment maneuver to maintain its nominal orbit by NASA on 27 February 2020, which may introduce biases that compromise the accuracy of quantitative time series analysis as the drift continues. Here, we evaluate the impact of Terra's orbital drift by comparing the differences between the Terra MODIS albedo and albedo products derived from Aqua MODIS, harmonized Landsat and Sentinel 2, Sentinel 3, and PROMICE (Programme for Monitoring of the Greenland Ice Sheet) ground measurements over the Greenland ice sheet. Our results suggest that the influence of orbital drift on albedo is small (+0.01 in 2020), but potentially biased for time series analysis. Our analysis also finds that the drift effect that causes earlier image acquisition time may lead to more apparently cloudy pixels and thus effectively reduce the Terra MODIS temporal resolution over Greenland.

Keywords

Aqua MODIS, Greenland, Greenland ice sheet, Harmonized Landsat, Landsat, MODIS, MODIS albedo, MODIS temporal resolution, NASA, PROMICE, Sentinel-2, Sentinel-3, Terra, accuracy, acquisition, acquisition time, adjustment maneuvers, albedo, albedo products, analysis, apparent effect, applications, aqua, bias, cloudy pixels, differences, drift, drift effects, effect, glaciological applications, ice sheet, image acquisition time, images, impact, inclination, influence, influence of orbital drift, maneuver, measurements, nominal orbit, orbit, orbital drift, pixel, production, quantitative time-series analysis, resolution, results, sentinel, series, series analysis, sheet, temporal consistency, temporal resolution, time, time series, time series analysis

Funders

  • European Research Council
  • European Commission

Data Provider: Digital Science