Abstract

Open and analysis-ready data, as well as methodological and technical advancements have resulted in an unprecedented capability for observing the Earth’s land surfaces. Over 10 years ago, Landsat time series analyses were inevitably limited to a few expensive images from carefully selected acquisition dates. Yet, such a static selection may have introduced uncertainties when spatial or inter-annual variability in seasonal vegetation growth were large. As seminal pre-open-data-era papers are still heavily cited, variations of their workflows are still widely used, too. Thus, here we quantitatively assessed the level of agreement between an approach using carefully selected images and a state-of-the-art analysis that uses all available images. We reproduced a representative case study from the year 2003 that for the first time used annual Landsat time series to assess long-term vegetation dynamics in a semi-arid Mediterranean ecosystem in Crete, Greece. We replicated this assessment using all available data paired with a time series method based on land surface phenology metrics. Results differed fundamentally because the volatile timing of statically selected images relative to the phenological cycle introduced systematic uncertainty. We further applied lessons learned to arrive at a more nuanced and information-enriched vegetation dynamics description by decomposing vegetation cover into woody and herbaceous components, followed by a syndrome-based classification of change and trend parameters. This allowed for a more reliable interpretation of vegetation changes and even permitted us to disentangle certain land-use change processes with opposite trajectories in the vegetation components that were not observable when solely analyzing total vegetation cover. The long-term budget of net cover change revealed that vegetation cover of both components has increased at large and that this process was mainly driven by gradual processes. We conclude that study designs based on static image selection strategies should be critically evaluated in the light of current data availability, analytical capabilities, and with regards to the ecosystem under investigation. We recommend using all available data and taking advantage of phenology-based approaches that remove the selection bias and hence reduce uncertainties in results.

Highlights

  • Earth observation (EO) data have long been used to monitor land cover, land cover change, and long-term modifications of the land surface [1,2,3,4]

  • All maps presented in the following are available through an interactive web viewer: https://ows.geo.hu-berlin.de/webviewer/crete/ accessed on 18 September 2021; note that the vegetation components map for 1984, i.e., the first year of available data, is incomplete as a full phenological cycle need to exist to extract land surface phenology (LSP) metrics

  • Net change over Crete is negative (Table 4) with 50% and 26% of semi-natural areas showing signs of vegetation decline and increase, respectively. Not numerically comparable, these numbers resemble the findings in Hostert et al [42], who found that over 40% of the mountain area of central Crete (Psiloritis) showed a decreasing trend of vegetation cover

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Summary

Introduction

Earth observation (EO) data have long been used to monitor land cover, land cover change, and long-term modifications of the land surface [1,2,3,4]. The available image metadata catalogs had to be meticulously screened concerning their foreseen application, e.g., considering cloud coverage, cloud distribution, solar angles, or seasonal suitability. This means that scientists aimed to buy as few as possible images with as high as possible quality. In rare circumstances were analyses performed on longer time series This was further cemented by the fact that computational power and storage capacities were limited, image processing software were often proprietary, expensive, and mostly distributed as “point-and-click” toolsets with nonautomated workflows, and a comparably low level of analysis-readiness of the acquired data. Technological and scientific advances have drastically changed the way EO data are being used since [13], only very recently, the full depth of the standardized USGS archive became accessible over Europe (i.e., this study’s area of interest)

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