Francesco Zignol, Erik Kjellström, Kristoffer Hylander, Biruk Ayalew, Beyene Zewdie, Alejandro Rodríguez-Gijón, Ayco J. M. Tack
The dataset contains high spatial resolution maps showing monthly and annual averages of daily maximum temperature, daily minimum temperature, and daily mean relative humidity for the Jimma zone in southwestern Ethiopia. The maps were created by using statistical downscaling applied to widely used reanalysis data for the period 1979 – 2020 and climate projections from a combination of different global climate models (GCMs) and scenarios (SSPs; Shared Socioeconomic Pathways) for the period 2021 – 2100.
The aim of creating the dataset was to investigate how climate change affects the understory microclimate in forests and agroforests, which can help develop sustainable and climate-smart farms and landscape-level adaptations within coffee agroforestry systems. Results obtained from analyses of the maps are discussed in a published case study of Arabica coffee in its native range.
The dataset includes 42,198 maps in GeoTIFF format, covering an area of about 67×50 km at a spatial resolution of 30×30 m. The full set of maps, as well as specific subsets of the maps, can be downloaded here. Moreover, the map content is shown in an interactive graphical presentation where the user can select a desired climate variable, scenario, and model, and see how the climate changes with time.
Terrestrial Model simulations Microclimate Temperature Humidity Southwestern Ethiopia Jimma ERA5 data GCM and emission scenarios Predictions Agroforestry Climate change Forest understory Statistical downscaling
In the article by Zignol et al. (2023), based on this data set, we created maps of the future microclimate, and we concluded that coffee farming might have to relocate to higher elevations due to increasing temperatures. In these maps you can, for example, see that the temperature increase over time is larger at lower elevations (northeastern part in the maps) than at higher elevations (central western part in the maps), as well as along roads and forest edges.
Other patterns you can see are that changes in maximum temperature are larger than changes in minimum temperature, and that the increase in temperature seems largest in the period April to June. Analyzing and comparing spatiotemporal patterns in projected maps can help us understand that climate change is not uniform, and can in this particular landscape help to design different strategies for climate adaptation in different parts of the landscape.
Overview of the study area in Jimma zone, southwestern Ethiopia. Displayed in the top right is an inset map of Ethiopia, with the study area northwest of Jimma indicated by a white rectangular box. Elevation is shown only for the area covered by trees (forests and agroforests), where microclimate is modelled. The figure is identical to Figure 1 in the article by Zignol et al. (2023). Reproduced under a CC-BY 4.0 licence.
You can download the full set of maps with climate predictions, or download the maps related to a specific climate model and emission scenario. What you download are GeoTIFF files that are useful for the visualization of a certain climate variable under a certain scenario, or be used in GIS-environments for other future studies.
To easily see the patterns discussed by Zignol et al. (2023) as well as other patterns you can, in the interactive data visualization below, select your favorite model, the emission scenario, and the climate variable you are most interested in. Then you can use an image slider to see how that variable changes with time and in space over the predicted period. What you see in the viewer are JPEG image files that have been created from the GeoTIFF files.
The dataset is arranged in a file tree structure with three main directories, one for each climate variable.
Under each main directory, all available GeoTIFF files for each combination of climate model and climate scenario are provided, compressed into one single zip file per combination.
Explanations of file content and file naming rules are given in the section Data description, together with abbreviations for models and scenarios.
You can download individual zip files by selecting in the file list below.
Alternatively, you can download all data files by clicking on the link below the file list.
Because of the large data volume (156 GiB, 42 files), downloading all files can take can take long time and requires sufficent disk space on your system.
Click on the categories below to view the files. Click on a file link to download a selected file. Or, click on the link below the file list to download all data files.
Here, you can select and view a map with the climate prediction for a given year. For this, select your favorite model, an emission scenario or the past, and the climate variable you are most interested in. Also, select either a specific month for averaging or annual averaging. The default choice is annual averaging.
Use the slider to move forwards or backwards in time.
Abbreviations for models and scenarios are explained in the Data description section.
Please, note that some combinations of model, scenario and timepoint are not possible. This is for the following reasons:
An attempt to choose an impossible combination will result in an error message being shown instead of a map.
Francesco Zignol, Erik Kjellström, Kristoffer Hylander, Biruk Ayalew, Beyene Zewdie, Alejandro Rodríguez-Gijón, Ayco J. M. Tack (2024) Maps of past and simulated future microclimate in forests and agroforests in southwestern Ethiopia, 1979 – 2100. Dataset version 1. Bolin Centre Database. https://doi.org/10.17043/zignol-2024-sw-ethiopia-microclimate-1
Hersbach, H., Bell, B., Berrisford, P., Hirahara, S., Horányi, A., Muñoz-Sabater, J., Nicolas, J., Peubey, C., Radu, R., Schepers, D., Simmons, A., Soci, C., Abdalla, S., Abellan, X., Balsamo, G., Bechtold, P., Biavati, G., Bidlot, J., Bonavita, M., De Chiara, G., Dahlgren, P., Dee, D., Diamantakis, M., Dragani, R., Flemming, J., Forbes, R., Fuentes, M., Geer, A., Haimberger, L., Healy, S., Hogan, R.J., Hólm, E., Janisková, M., Keeley, S., Laloyaux, P., Lopez, P., Lupu, C., Radnoti, G., de Rosnay, P., Rozum, I., Vamborg, F., Villaume, S., Thépaut, J.-N., 2020. The ERA5 global reanalysis. Q. J. R. Meteorol. Soc. 146, 1999–2049. https://doi.org/10.1002/qj.3803
Müller, W.A., Jungclaus, J.H., Mauritsen, T., Baehr, J., Bittner, M., Budich, R., Bunzel, F., Esch, M., Ghosh, R., Haak, H., Ilyina, T., Kleine, T., Kornblueh, L., Li, H., Modali, K., Notz, D., Pohlmann, H., Roeckner, E., Stemmler, I., Tian, F., Marotzke, J., 2018. A Higher-Resolution version of the Max Planck Institute Earth System Model (MPI-ESM1.2-HR). J. Adv. Model. Earth Syst. 10, 1383–1413. https://doi.org/10.1029/2017MS001217
Riahi, K., van Vuuren, D.P., Kriegler, E., Edmonds, J., O’Neill, B.C., Fujimori, S., Bauer, N., Calvin, K., Dellink, R., Fricko, O., Lutz, W., Popp, A., Cuaresma, J.C., Kc, S., Leimbach, M., Jiang, L., Kram, T., Rao, S., Emmerling, J., Ebi, K., Hasegawa, T., Havlik, P., Humpenöder, F., Da Silva, L.A., Smith, S., Stehfest, E., Bosetti, V., Eom, J., Gernaat, D., Masui, T., Rogelj, J., Strefler, J., Drouet, L., Krey, V., Luderer, G., Harmsen, M., Takahashi, K., Baumstark, L., Doelman, J.C., Kainuma, M., Klimont, Z., Marangoni, G., Lotze-Campen, H., Obersteiner, M., Tabeau, A., Tavoni, M., 2017. The Shared Socioeconomic Pathways and their energy, land use, and greenhouse gas emissions implications: An overview. Glob. Environ. Change 42, 153–168. https://doi.org/10.1016/j.gloenvcha.2016.05.009
Seland, Ø., Bentsen, M., Olivié, D., Toniazzo, T., Gjermundsen, A., Graff, L.S., Debernard, J.B., Gupta, A.K., He, Y.-C., Kirkevåg, A., Schwinger, J., Tjiputra, J., Aas, K.S., Bethke, I., Fan, Y., Griesfeller, J., Grini, A., Guo, C., Ilicak, M., Karset, I.H.H., Landgren, O., Liakka, J., Moseid, K.O., Nummelin, A., Spensberger, C., Tang, H., Zhang, Z., Heinze, C., Iversen, T., Schulz, M., 2020. Overview of the Norwegian Earth System Model (NorESM2) and key climate response of CMIP6 DECK, historical, and scenario simulations. Geosci. Model Dev. 13, 6165–6200. https://doi.org/10.5194/gmd-13-6165-2020
Swart, N.C., Cole, J.N.S., Kharin, V.V., Lazare, M., Scinocca, J.F., Gillett, N.P., Anstey, J., Arora, V., Christian, J.R., Hanna, S., Jiao, Y., Lee, W.G., Majaess, F., Saenko, O.A., Seiler, C., Seinen, C., Shao, A., Sigmond, M., Solheim, L., von Salzen, K., Yang, D., Winter, B., 2019. The Canadian Earth System Model version 5 (CanESM5.0.3). Geosci. Model Dev. 12, 4823–4873. https://doi.org/10.5194/gmd-12-4823-2019
Zignol, F., Kjellström, E., Hylander, K., Ayalew, B., Zewdie, B., Rodríguez-Gijón, A., Tack, A.J.M., 2023. The understory microclimate in agroforestry now and in the future – a case study of Arabica coffee in its native range. Agric. For. Meteorol. 340, 109586. https://doi.org/10.1016/j.agrformet.2023.109586
The dataset includes 42,198 maps in GeoTIFF format, together amounting to ca. 180 GB of data (uncompressed).
The maps cover an area of about 67×50 km in southwestern Ethiopia (Jimma zone) and have a spatial resolution of 30×30 m. The projected coordinate system for all maps is WGS 1984 UTM zone 37N.
Our study focuses only on the forest-covered part (44% of the entire study area), which encompasses 1,645,794 pixels (1481 km²). Thus, climate variables are only estimated for these pixels.
We estimated monthly (12) and annual (1) averages of three climate variables for the period 1979 – 2100:
The data for the three climate variables is always stored to two decimal places (e.g., 28.45°C for maximum temperature, 19.72°C for minimum temperature, 83.67% for relative humidity).
For past estimates (1979 – 2020), we used the fifth generation ECMWF reanalysis for the global climate and weather for the past decades (ERA5; Hershbach et al. 2020).
For future projections (2021– 2100) we used outputs from three different global climate models (GCMs) under different emission scenarios, i.e., predictions of the rate at which we continue to release greenhouse gases into the atmosphere.
We used output data from three CMIP6 GCMs spanning a range of equilibrium climate sensitivity (ECS):
We considered multiple Shared Socioeconomic Pathways (SSPs; Riahi et al. 2017), ranging from a more sustainable, very low emission scenario (SSP1-1.9; CO₂ emissions cut to net zero around 2050) to a fossil fuel oriented, very high emission scenario (SSP5-8.5; CO₂ emissions close to triple by 2075). Note that SSP1-1.9 is available only for CanESM5.
The dataset is arranged in a file tree structure with three main directories, one for each climate variable.
Under each main directory, all available GeoTIFF files for each combination of climate model and climate scenario are provided, compressed into one single zip file per combination. The following abbreviations are used in zip file names:
Tmx
maximum temperatureTmn
minimum temperatureRhm
relative humidityCan5
CanESM5ERA5
ERA5mpi1
MPI-ESM1.2-HRNor2
NorESM2119
SSP1-1.9126
SSP1-2.6245
SSP2-4.5370
SSP3-7.0585
SSP5-8.5The individual tif
files have names that also identify the year (1979
to 2100
) and time averaging period (00
to 12
; where 00
denotes annual average and 01
to 12
the monthly averages).
We have published a scientific paper on the impact of climate change on the microclimate in forests and agroforests in southwestern Ethiopia (Zignol et al. 2023). The title of the paper was The understory microclimate in agroforestry now and in the future – a case study of Arabica coffee in its native range.
The aim of this paper was to investigate how climate change affects the understory microclimate in forests and agroforests, which can help develop sustainable and climate-smart farms and landscape-level adaptations within coffee agroforestry systems.
While the paper was a major scientific advance, we could only show a small subset of the data and in poor resolution. To ensure that the full data set is published and available to the scientific community and local stakeholders in Ethiopia, we provide all maps for download here. Moreover, we also provide an interactive visualization of microclimate changes that is informative in itself and complement the paper in illustrating the projected changes across this landscape.
The GeoTIFF (.tif
) files are useful for the visualization of a certain climate variable under a certain scenario and can be used in GIS-environments for other future studies.
The associated interactive graphical presentation of the map content shows JPEG image files, with one unique .jpg
file corresponding to each unique .tif
file. All .jpg
files for one specific climate variable have the same colour scheme, which is explained below the graphical presentation. Individual JPEG image files can be downloaded from the graphical presentation. Select a desired image and use your browser's standard way to save an image file.
Francesco Zignol
Department of Forest Ecology and Management
Swedish University of Agricultural Sciences
SE-901 83 Umeå
Sweden
Earth science services > Data analysis and visualization
Continent > Africa > Eastern Africa > Ethiopia
English
Bolin Centre Database
1
10.17043/zignol-2024-sw-ethiopia-microclimate-1
2024-10-28 18:56:10