A large proportion of dryland trees and shrubs (hereafter referred to collectively as trees) grow in isolation, without canopy closure. These non-forest trees have a crucial role in biodiversity, and provide ecosystem services such as carbon storage, food resources and shelter for humans and animals1,2. However, most public interest relating to trees is devoted to forests, and trees outside of forests are not well-documented3. Here we map the crown size of each tree more than 3 m2 in size over a land area that spans 1.3 million km2 in the West African Sahara, Sahel and sub-humid zone, using submetre-resolution satellite imagery and deep learning4. We detected over 1.8 billion individual trees (13.4 trees per hectare), with a median crown size of 12 m2, along a rainfall gradient from 0 to 1,000 mm per year. The canopy cover increases from 0.1% (0.7 trees per hectare) in hyper-arid areas, through 1.6% (9.9 trees per hectare) in arid and 5.6% (30.1 trees per hectare) in semi-arid zones, to 13.3% (47 trees per hectare) in sub-humid areas. Although the overall canopy cover is low, the relatively high density of isolated trees challenges prevailing narratives about dryland desertification5,6,7, and even the desert shows a surprisingly high tree density. Our assessment suggests a way to monitor trees outside of forests globally, and to explore their role in mitigating degradation, climate change and poverty.
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Global tree cover maps are available at http://earthenginepartners.appspot.com/science-2013-global-forest. CHIRPS rainfall data are freely available at the Climate Hazard Group (https://www.chc.ucsb.edu/data/chirps). The Copernicus land-use map can be downloaded at https://land.copernicus.eu/global/. Commercial very-high-resolution satellite images were acquired by NASA, under a NextView Imagery End User Licence Agreement. The copyright remains with DigitalGlobe, and redistribution is not possible. However, the derived products produced in this Article are made publicly available at the Oak Ridge National Laboratory at https://doi.org/10.3334/ORNLDAAC/1832. Any further relevant data are available from the corresponding authors upon reasonable request.
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We thank Maxar for providing commercial satellite data through the NextView Imagery End User Licence Agreement of the National Geospatial Intelligence Agency. This research is part of the Blue Waters sustained peta-scale computing project, which is supported by the National Science Foundation (awards OCI-0725070 and ACI-1238993), the State of Illinois and—as of December 2019—the National Geospatial-Intelligence Agency. Blue Waters is a joint effort of the University of Illinois at Urbana-Champaign and its National Center for Supercomputing Applications. M.B. was financed by an AXA post-doctoral research grant and a DFF Sapere Aude grant (9064-00049B). A.K. and J. Schöning were funded by a Lichtenberg Professorship of the Volkswagen Foundation. J.C. acknowledges ANR grants (CEBA, ref. ANR-10-LABX-25-01 and TULIP: ANR-10-LABX-0041). We acknowledge support by the Villum Foundation through the project ‘Deep Learning and Remote Sensing for Unlocking Global Ecosystem Resource Dynamics’ (DeReEco). L.V.R. was funded by the European Research Council (ERC) under the European Union’s Horizon 2020 research and innovation programme (grant agreement no. 853222 FORESTDIET). This Article contributes to the Global Land Programme, glp.earth. We thank the group around M. Hansen for making their product on global tree cover freely available; T. Lee for suggesting this project; K. Murphy for his support; D. Duffy for his high-performance computing support; S. Keesey, C. Williamson, C. Crittenden, K. Allen, M. Schlenk, B. Bates and K. Peterman for their satellite data contributions; and W. Kramer and B. Bode for their high-performance computing support. Approved for public release, no. 20-732.
The authors declare no competing interests.
Peer review information Nature thanks Niall Hanan, Liming Zhou and the other, anonymous, reviewer(s) for their contribution to the peer review of this work.
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Extended data figures and tables
This set of 256 × 256-pixel plots from the independent test dataset shows the capabilities of the convolutional neural network model to predict trees (right column) from panchromatic images (left column) and NDVI (central column) at 0.5-m resolution.
a, Manually labelled tree crowns from the independent test dataset are compared against predictions. The comparison is done for 100 random plots each having 256 × 256 pixels. Here, the canopy area (in m2) of the trees in the plots is compared. b, As in a, but for the density (the number of labelled or predicted trees per plot). c, As in a, but for mean crown size per plot. d, The crown sizes of 102 in situ measured trees from 2 field campaigns in Senegal (Extended Data Fig. 4) are compared with the predicted ones. Extended Data Table 2 provides more details. n = 100 plots with 256 × 256-pixel size.
a, Before training the model, the spaces between labelled tree crowns (light blue) were filled (red) and given a higher weight. During training, the model was penalized more strongly for wrongly classifying gap pixels compared to other misclassifications. As a result, tree crowns that touch or are close to each other could be reliably separated. b, Examples of predicted trees (green), showing that most trees standing close to each other were mapped as individuals trees.
The study area for the wall-to-wall mapping is the westernmost part of the Sahara and Sahel. It represents a typical north–south ecological and climatic gradient, starting in the Sahara Desert in hyper-arid areas (rainfall of 0–150 mm yr−1) with a sparse vegetation coverage, over arid (rainfall of 150–300 mm yr−1) and semi-arid (rainfall of 300–600 mm yr−1) Sahelian rangelands and croplands, up to sub-humid (rainfall of 600–1,000 mm yr−1) Sudanian lands, where shrublands turn into forests. a, The locations of the manually drawn 89,899 tree crowns used for training the model are shown in red. CHIRPS rainfall43 was used to delineate the rainfall zones. The land use for farmland and urban is from Copernicus Global Land26. In situ data were collected at the field sites around Widou and Dahra in Senegal. Areas of insufficient data quality and beyond rainfall of 1,000 mm yr−1 were masked. b, The region was analysed for sandy (>70% sand content) and non-sandy areas44.
a, The density of trees with a crown size larger 3 m2 per hectare. b, The canopy cover. c, Mean crown size. All variables were mapped by 100 × 100-m (1-ha) grids. Rainfall isohyets of 150, 300, 600 and 1,000 mm yr−1 are also shown.
a–d, The tree density per hectare is shown for different crown size classes: 3–15 m2 (a), 15–50 m2 (b), 50–200 m2 (c), and >200 m2 (d). Trees in the class >200 m2 typically do not represent individual tree crowns, but instead reflect closed-canopy areas. Trees <3 m2 are not shown, owing high uncertainty in this class.
a, Canopy cover of the study area from ref. 8. b, Field-measured crown diameter (derived from crown size 3–200 m2) of 811 individual trees measured in situ in the Ferlo of Senegal21. The y-axis has been log-transformed. c, As in b, but for the crown size and without log transformation. d, Woody cover derived from individual trees differs from the current state-of-the-art tree cover map from ref. 19. n = 4,017 grids; r2 = 0.28.
We used 11,128 multispectral images from the QuickBird-2, GeoEye-1, WorldView-2 and WorldView-3 satellites, acquired from November to March of 2005–2018. Priority was set to images from the early dry season (starting in November), and an off-nadir angle of <25°. Although the model has been trained and validated to work for late-dry season images, the uncertainty is higher in February and March. a, Image acquisition months. b, Sun azimuth at the image acquisition time. c, Off-nadir angle shown for each image.
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Brandt, M., Tucker, C.J., Kariryaa, A. et al. An unexpectedly large count of trees in the West African Sahara and Sahel. Nature 587, 78–82 (2020). https://doi.org/10.1038/s41586-020-2824-5
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