open access publication

Article, Early Access, 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, 2666-0172, Volume 9, 10.1016/j.srs.2023.100116

Contributors

Feng, Shunan 0000-0002-8534-3066 (Corresponding author) [1] Wehrle, Adrien [2] [3] Cook, Joseph Mitchell [1] Anesio, Alexandre Magno [1] Box, Jason E 0000-0003-0052-8705 [4] Benning, Liane G. [3] [5] [6] Tranter, Martyn (Corresponding author) [1]

Affiliations

  1. [1] Aarhus Univ, Dept Environm Sci, Frederiksborgvej 399, DK-4000 Roskilde, Denmark
  2. [NORA names: AU Aarhus University; University; Denmark; Europe, EU; Nordic; OECD];
  3. [2] Univ Zurich, Inst Geog, CH-8052 Zurich, Switzerland
  4. [NORA names: Switzerland; Europe, Non-EU; OECD];
  5. [3] Free Univ Berlin, Dept Earth Sci, D-12249 Berlin, Germany
  6. [NORA names: Germany; Europe, EU; OECD];
  7. [4] Geol Survey Denmark & Greenland, Copenhagen, Denmark
  8. [NORA names: GEUS Geological Survey of Denmark and Greenland; Governmental Institutions; Denmark; Europe, EU; Nordic; OECD];
  9. [5] GFZ German Res Ctr Geosci, Sect Interface Geochem, D-14473 Potsdam, Germany
  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

Albedo, Google Earth Engine, Greenland ice sheet, MODIS, Orbit drift, Time series

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