Satellite observations reveal a decreasing albedo trend of global cities over the past 35 years

Shengbiao Wu, Xingwen Lin, Zunjian Bian, Mathew Lipson, Raffaele Lafortezza, Qiang Liu, Sue Grimmond, Erik Velasco, Andreas Christen, Valéry Masson, Ben Crawford, Helen Claire Ward, Nektarios Chrysoulakis, Krzysztof Fortuniak, Eberhard Parlow, Wlodzimierz Pawlak, Nigel Tapper, Jinkyu Hong, Je Woo Hong, Matthias RothJiafu An, Chen Lin, Bin Chen

Research output: Contribution to journalArticlepeer-review

10 Citations (Scopus)

Abstract

Urban surface albedo is an essential biophysical variable in the surface energy balance across all scales, from micro-scale (materials) to the globe, changing with land covers and three-dimensional structures over urban areas. Urban albedos are dynamic over space and time but have not yet been quantified over global scales due to the lack of high-resolution albedo datasets. Here, we combined the direct estimation approach and Landsat surface reflectance product to generate a 30-m-resolution annual surface albedo dataset for 3037 large cities (area > 50 km2) worldwide for the period from 1986 to 2020, allowing spatial patterns and long-term temporal trends to be explored with possible causal drivers, and quantification of the surface radiative forcing from these albedo changes. Evaluation of this new albedo dataset using global urban flux tower-based measurements demonstrates its high accuracy with an overall bias and root-mean-square-error (RMSE) of 0.005 and 0.025, respectively. Analysis of the dataset reveals an overall decreasing trend of albedo during the 35-year evaluation period (1986–2020), which is robust accounting for uncertainties from training sample representativeness, Landsat data uncertainty, seasonal variation, and snow-cover contamination. Our results reveal that urban greening (measured by the positive Normalized Difference Vegetation Index (NDVI) trend) can well explain the total variances in the albedo trend for the 35-year period through two different pathways of tree planting and urban warming-enhanced vegetation growth. The decrease in urban albedo caused a warming effect indicated by positive surface radiative forcing, with a global city-level average surface radiative forcing of 2.76 W·m−2. These findings enhance our understanding of urbanization's impacts on albedo-related biophysical processes and can provide information to quantify urban surface radiation energy and design effective mitigation strategies to reduce urban warming.

Original languageEnglish
Article number114003
JournalRemote Sensing of Environment
Volume303
DOIs
Publication statusPublished - 2024 Mar 15

Bibliographical note

Publisher Copyright:
© 2024 Elsevier Inc.

All Science Journal Classification (ASJC) codes

  • Soil Science
  • Geology
  • Computers in Earth Sciences

Fingerprint

Dive into the research topics of 'Satellite observations reveal a decreasing albedo trend of global cities over the past 35 years'. Together they form a unique fingerprint.

Cite this