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2,591 results for “remotization”

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zenodo44/100

Remote Sensing based Sea Surface partial pressure of CO2 (pCO2) and air-sea CO2 flux (FCO2) in the East China Sea (2003-2019)

<p>Based on <em>in situ</em> seawater <em>p</em>CO<sub>2</sub> data collected on 51 cruises/legs over the past two decades, a satellite retrieval algorithm for seawater <em>p</em>CO<sub>2</sub> was developed by combining the semi-mechanistic algorithm and machine learning method (MeSAA-ML). MeSAA-ML introduces semi-analytical parameters, including the temperature-dependent seawater <em>p</em>CO<sub>2</sub> (<em>p</em>CO<sub>2,therm</sub> ) and upwelling index (<em>UI<sub>SST</sub></em>), to characterise the combined effect of atmospheric CO<sub>2</sub> forcing, thermodynamic effects, and multiple mixing processes on seawater <em>p</em>CO<sub>2</sub>. Additionally, considering the biological effects and various sub-regional features, multiple ocean colour parameters were also used as inputs in XGBoost, the best-selected machine learning algorithm. Independent cruise-based data were used to validate the satellite-derived <em>p</em>CO<sub>2</sub>, which achieved excellent performance in this complicated marginal sea, with low root mean square error (RMSE=19.6 &mu;atm) and mean absolute percentage deviation (APD=4.12%). Air-sea CO2 fluxes are calculated based on retrieved seawater <em>p</em>CO<sub>2</sub>.&nbsp;</p>

opencc-by-4.0Mar 2023View details →
zenodo44/100

FESOM-REcoM model data: A regime shift on Weddell Sea continental shelves with local and remote physical-biogeochemical implications is avoidable in a 2°C scenario

<p>This data set includes the minimal data necessary to reproduce the findings of Nissen et al. (2023). Output of model simulations with the global ocean biogeochemical model FESOM1.4-REcoM2 is provided. In particular, besides information on the model grid, the data set includes&nbsp;annual mean&nbsp;water mass properties (temperature, salinity, density, oxygen, pH) and freshwater fluxes from sea ice and ice shelves&nbsp;and&nbsp;decadal averages of air-sea CO2 fluxes and deep-ocean carbon accumulation rates.&nbsp;Model results are provided from 1980-2100 for the four emission scenarios SSP1-2.6, SSP2-4.5, SSP3-7.0, and SSP5-8.5 (sorted from low emission to high emission).</p> <p>Please see README for more information on the individual files.&nbsp;</p> <p>Data set belongs to:&nbsp;</p> <p>Nissen, C., R. Timmermann, M. Hoppema, and J. Hauck, 2023: A regime shift on Weddell Sea continental shelves with local and remote physical-biogeochemical implications is avoidable in a 2&deg;C scenario.&nbsp;<em>J. Climate</em>,&nbsp;<a href="https://doi.org/10.1175/JCLI-D-22-0926.1">https://doi.org/10.1175/JCLI-D-22-0926.1</a>, in press.</p>

opencc-by-4.0Jul 2023View details →
zenodo44/100

Bayesian Analysis for Remote Biosignature Identification on exoEarths (BARBIE) I: Using Grid-Based Nested Sampling in Coronagraphy Observation Simulations for H2O

<p>We present all of the data across our SNR and abundance study for the molecule H2O for an exoEarth twin. The wavelength range is from 0.515-1 micron, with 25 evenly spaced 20% bandpasses in this range. The SNR ranges from 3-16, and the abundance values range from log10(VMR)&nbsp;&nbsp;= -3.5&nbsp;to -1.5 in steps of 0.5 and 0.25 (all presented in VMR in the associated table). We&nbsp;present the lower and upper wavelength per bandpass, the input H2O value (abundance case), the retrieved H2O value (presented as the log10(VMR)), the lower and upper limits of the 68% credible region&nbsp;(presented as the log10(VMR)), and the log-Bayes factor for H2O. For more information about how these were calculated, please see&nbsp;Bayesian Analysis for Remote Biosignature Identification on exoEarths (BARBIE) I: Using Grid-Based Nested Sampling in Coronagraphy Observation Simulations for H2O, accepted and currently available on arXiv.&nbsp;</p> <p>To open this csv as a Pandas dataframe, use the following command:</p> <p>your_dataframe_name = pd.read_csv(f&#39;zenodo_table.csv&#39;, dtype={&#39;Input H2O&#39;: str})</p>

opencc-by-4.0Jul 2023View details →
zenodo44/100

Remotely sensed geoarchaeological marks in the hinterland of Ravenna

<p>GeoPackage database with 994 fluvial and anthropogenic traces mapped in the hinterland of Ravenna through historical imagery, satellite images and drone photos, together with related metadata.</p> <p>&nbsp;</p> <p>Sources of aerial and satellite images analysed include:</p> <ul> <li>Istituto Geografico Militare Italiano (IGMI), Volo GAI (Gruppo Aeronautico Italiano) aerial photos are available at https://servizimoka.regione.emilia-romagna.it/mokaApp/apps/VIGMIGAI1954_H5/index.html (last accessed on 31 January 2025).</li> <li>Ministero dell'Ambiente e della Tutela del Territorio e del Mare (MATTM) aerial photos are available at http://www.pcn.minambiente.it/viewer/ (last accessed on 31 January 2025).</li> <li>Agenzia per le Erogazioni in Agricoltura (AGEA) aerial photos are available at https://servizimoka.regione.emilia-romagna.it/mokaApp/apps/CORERH5/index.html (last accessed on 31 January 2025).</li> <li>Google Earth satellite images, accessed through Google Earth Pro for desktop, which can be downloaded from https://www.google.it/earth/versions/ (last accessed on 31 January 2025).</li> <li>Microsoft Bing satellite images are available at https://www.bing.com/maps/aerial (last accessed on 31 January 2025). Historical imagery has been accessed through a third-party website freely available at https://zoom.earth/, but this service has been discontinued (last accessed on 31 January 2025).</li> <li>Esri World Imagery satellite images are available at https://livingatlas.arcgis.com/wayback/ (last accessed on 31 January 2025).</li> <li>Consorzio Telerilevamento Agricoltura (TeA) are available at https://servizimoka.regione.emilia-romagna.it/mokaApp/apps/CORERH5/index.html (last accessed on 31 January 2025).</li> <li>Compagnia Generale Riprese Aeree (CGR) are available at https://servizimoka.regione.emilia-romagna.it/mokaApp/apps/CORERH5/index.html (last accessed on 31 January 2025).</li> <li>PlanetScope satellite images were made available through Planet Education and Research Program: more information is available at https://www.planet.com/industries/education-and-research/ (last accessed on 31 January 2025).</li> </ul>

opencc-by-4.0Sep 2023View details →
zenodo44/100

Supplement to "Low-level mixed-phase clouds at the high Arctic site of Ny-Ålesund: A comprehensive long-term dataset of remote sensing observations"

<p>This dataset is a supplement to "Low-level mixed-phase clouds at the high Arctic site of Ny-&Aring;lesund: A comprehensive long-term dataset of remote sensing observations", available at <a href="http://doi.org/10.5281/zenodo.7803064">doi.org/10.5281/zenodo.7803064</a>. The additional variables here included are: slow edge velocity, fast edge velocity, and eddy dissipation rate (EDR). All variables are stored on the same time and range grids adopted for the main dataset. Similarly, the event selection and file structure are identical to those of the main dataset.<br><br>Slow and fast edge velocities are derived from Doppler spectra recorded by the zenith-pointing 94-GHz cloud radar. The slow (fast) edge velocity is calculated as the velocity associated with the slowest (fastest) Doppler bin above the peak noise level, belonging to a spectral cluster whose width is at least 5 Doppler bins.<br><br>The EDR is retrieved following the approach by Borque et al. (2016; <a href="http://doi.org/10.1002/2015JD024543">doi.org/10.1002/2015JD024543</a>), using as input the slow edge velocity, and model horizontal wind speed from the main dataset. EDR is retrieved in 5 minute intervals, up to a maximum range of 3 km.<br><br>The detailed documentation of the variables here included can be found in the Supporting Information to the following publication: <a href="https://doi.org/10.1029/2023GL106599" target="_blank" rel="noopener">doi.org/10.1029/2023GL106599</a>.</p>

opencc-by-4.0Sep 2023View details →
edi44/100

Photosynthetically Active Radiation data taken with the Delta-T SunScan wand every 15 cm of 1m x 1m chamber flux and point frame plots as well as four remotely monitored canopies at the Toolik Field Station in AK, Summer 2012.

Within-canopy PAR was measured with a Delta-T SunScan wand every 15 cm from the ground to above the canopy under both direct and diffuse light. The data includes all outputs from the SunScan wand: time of measurement, spread of PAR sensors, total irradiance, total diffuse light, and individual outputs of 64-PAR sensors on the SunScan wand. These measurements were taken for 1m x 1m chamber flux (n=14) and point frame (n=19) plots as well as sites four montitored remotely by PAR sensors located above, within, and below shrub canopies. All plots were dominated either by tall Salix pulchra and Betula nana species and were located near the LTER shrub plots at Toolik Field Station , AK in the summer of 2012.

openOpenDec 2015View details →
edi44/100

Pond Area Estimates: Nine Study Regions in Alaska for 3 time periods (1950s, 1978-1982, 1999-2001) using remotely sensed images

The data are ArcGIS shapefiles by USGS quadrangle within 9 study regions: Arctic Coastal Plain, Stevens Village area, Yukon Flats, Minto Flats, Denali Flats, Talkeetna, Innoko Flats, Tetlin Flats, and Copper River Basin. Each shapefile polygon represents the shoreline of a pond as visually interpreted from each georectified remotely sensed image. All images were rectified based on at least 25 control points from 1:63 360 USGS digital raster graphics topographic maps using a second-order polynomial with a RMS error of less than one satellite image pixel (30 meters). All closed-basin ponds greater than 0.2 hectares were visually delineated and manually traced as polygons using ArcGIS. Each pond polygon has an ID and Hectares field representing the pond ID and area in hectares for the time period of the remotely sensed image.

openOpenDec 2008View details →
edi44/100

Tree ring, leaf mining, climate, and remote sensing data from aspen leaf miner survey sites: III - Climate, leaf mining, and NDVI data

This dataset contiains annual site-level measurements from 2004 - 2015 of growing season climate moisture index ( GS CMI; summed CMI from May - September), average site level leaf mining, and mean July - August normalized difference vegetation index (NDVI) derived from Landsat, GIMMS3g, MODIS Aqua, and MODIS Terra

openOpenMay 2019View details →
edi44/100

MCR LTER: Reference: Satellite Remote Sensing: Landsat ETM from 2001 to 2010

This LTER Remote Sensing spatial raster dataset consists of Landsat Enhanced Thematic Mapper image data collected between 2001 and 2010 over the island of Moorea and Tahiti. These are reference data, from the USGS EROS archive, not data generated by MCR LTER. This product was created by the U.S. Geological Survey (USGS) and contains Landsat data files in Geographic Tagged Image-File Format (GeoTIFF). NASA Landsat Program, 2009, Landsat ETM+ scene 20010429-LE70540722001119EDC00, LPGS_11.2.1, USGS, Sioux Falls, 04/29/2001.

openCustomFeb 2012View details →
edi44/100

MCR LTER: Reference: Satellite Remote Sensing: Landsat 7 in 1999 and 2000

This LTER Remote Sensing spatial raster dataset consists of Landsat 7 Thematic Mapper image data collected in 1999 and 2000 over the island of Moorea and Tahiti. These are reference data, from the USGS EROS archive, not data generated by MCR LTER. This product was created by the U.S. Geological Survey (USGS) and contains Landsat data files in Geographic Tagged Image-File Format (GeoTIFF). NASA Landsat Program, 2001, Landsat ETM+ scene RNL71054072_07220000426, Unspecified processing, USGS, Sioux Falls, 04/26/2000. NASA Landsat Program, 2003, Landsat ETM+ scene L7054072_19990830, Ortho product, USGS, Sioux Falls, 08/30/1999.

openCustomFeb 2012View details →
edi44/100

MCR LTER: Reference: Satellite Remote Sensing: Landsat MSS in 1979

This LTER Remote Sensing spatial raster dataset consists of Landsat Multi-Spectral Scanner (MSS) image data collected in 1979 over the island of Moorea and Tahiti. These are reference data, from the USGS EROS archive, not data generated by MCR LTER. This product was created by the U.S. Geological Survey (USGS) and contains Landsat data files in Geographic Tagged Image-File Format (GeoTIFF). NASA Landsat Program, 2010, Landsat MSS scene L3057072_07219790206_MTL, LPGS_11.2.1, USGS, Sioux Falls, 1979-02-06.

openCustomFeb 2012View details →
zenodo40/100

Hubei STEC Data through CORS stations for DOY 059 and 061 of the year 2018 which used in (Using Real GNSS Data for Ionospheric Disturbance Remote Sensing Associated with Strong Thunderstorm over Wuhan City, manuscript submitted to Earth and Space Science Journal AGU)

<p>Manuscript submitted to Earth and Space Science AGU entitled with&nbsp;<br> (Using Real GNSS Data for Ionospheric Disturbance Remote Sensing Associated with Strong Thunderstorm over Wuhan City)<br> by: Mohamed Freeshah, Xiaohong Zhang, Xiaodong Ren, Jun Chen, and Zhibo Zhao</p> <p>The STEC data inside two compressed folders named as stec059 and stec061, respectively.<br> The STEC file name has the CORS station name for the first forth letters and next three numbers epresent the Day of the year.<br> For example:<br> ES010590.18STEC<br> ES01 is the station name<br> 059 &nbsp;is the day of year (DOY), 2018</p>

opencc-by-4.0Apr 2020View details →
zenodo40/100

Isoprene in the Southern Ocean & remote sensed variables

<pre>%%%%%% Variables&#39; names contained in &quot;rodriguezrosetal_2020_isorems_data.csv&quot; %%%%%% &quot;id&quot; = source of the data (&quot;peg&quot; = PEGASO cruise, &quot;ace&quot; = ACE Expedition, &quot;pml&quot; = ANDREXII, &quot;ooki&quot; = Ooki et al. 2015, &quot;hack&quot; = Hackemberg et al. 2017) &quot;solar_time&quot; = solar time estimated with solaR package on R. &quot;month&quot; = month of the year. &quot;iso_pm&quot; = Isoprene concentration (pM) &quot;chla_fluo&quot; = Chlorophyll-a (fluorometric) &quot;chla_matchup&quot; = Chlorophyll-a (MODIS Aqua) &quot;sst_matchup&quot; = Sea Surface Temperature (MODIS Aqua) &quot;zeu_matchup&quot; = Depth of the Euphotic Layer (MODIS Aqua) &quot;poc_matchup&quot; = Particulate Organic Carbon (MODIS Aqua) &quot;pic_matchup&quot; = Particulate Inorganic Carbon (MODIS Aqua) &quot;mld_matchup&quot; = Mixing Layer Depth (Holte et al. 2017) &quot;par_matchup&quot; = PAR radiation (MODIS Aqua) &quot;lat&quot; = Latitude (decimal degrees) &quot;lon&quot; = Longitude (decimal degrees)</pre>

opencc-by-4.0Mar 2020View details →
zenodo40/100

Supplementary files for ground-based remote sensing of sesame drydown

<p>This is a collection of supplementary materials in support of the article entitled "Using normalized difference vegetation index to estimate sesame drydown and seed yield," which was published on Dec. 10, 2020 in Journal of Crop Improvement, 35:4, 508-521.&nbsp;</p> <p>Supplementary file 1 - list of computer program. This list documents Minitab macro, dryrate.mac, that was written to&nbsp;do regression analysis for sesame drydown data collected at the Texas A&amp;M&nbsp;AgriLife&nbsp;Research Center&nbsp;at Uvalde. The macro automates the process of running&nbsp;m x 9 linear regressions, where m represents the number of sesame plots/genotypes and 9 the number of vegetation indices.</p> <p>Supplementary file 2 - sample input data to macro dryrate.mac. The file contains nine vegetation indices measured five times from six plots during sesame drydown in the 2019 growing season.</p> <p>Supplementary file 3 - sample output data. This file&nbsp;contains the outputs of dryrate, including selected regression coefficients for<br>each of the six sesame plots.</p> <p>Supplementary file 4 - Figure S1. Scatter plots of average values of nine vegetation indices for 60 sesame genotypes measured five<br>times from 6 September 2019 to 6 October 2019.</p> <p>Supplementary file 5 - Table S1. Values of the slopes depicting the regressions between nine vegetation indices and time for 60 sesame genotypes.</p> <p>Supplementary file 6 - Table S2. Average values of different&nbsp;vegetation indices measured on Day 9 during drydown for 60 sesame<br>genotypes.</p> <p>Supplementary file 7 - Figure S2. Relationships between sesame seed yield and the slopes of regressions between nine vegetation indices and time during the drydown period.</p> <p>Supplementary file 8 - Figure S3. Histograms of the coefficients of determinations for the 60 linear regressions relating different<br>vegetation indices with time (days during sesame drydown).</p> <p>Supplementary file 9 - Figure S4. Ranking from the highest to the lowest of the maximum NDVI (normalized difference vegetation index) for the 60 sesame genotypes, along with the measured seed yields for the corresponding genotypes.<br>&nbsp;</p>

opencc-by-4.0Oct 2020View details →
zenodo40/100

Fast Remote Correlation Experiments for 1H Homonuclear Decoupling in Solids

<p>Experimental, pulse sequence and processing codes of the article &#39;&#39;Fast Remote Correlation Experiments for 1H Homonuclear Decoupling in Solids.&#39;&#39;published in JMR.</p> <p>Read the readme.rtf file for more information.</p>

opencc-by-4.0Oct 2020View details →
zenodo40/100

LimnoSat-US: A Remote Sensing Dataset for U.S. Lakes from 1984-2020

<p>LimnoSat-US is an analysis-ready remote sensing database that includes reflectance values spanning 36 years for 56,792 lakes across &gt; 328,000 Landsat scenes. The database comes pre-processed with cross-sensor standardization and&nbsp;the effects of clouds, cloud shadows, snow, ice, and macrophytes removed. In total, it contains over 22 million individual lake observations with an average of 393 +/- 233 (mean +/- standard deviation) observations per lake over the 36 year period.&nbsp; The data and code contained within this repository are as follows:</p> <p><em>HydroLakes_DP.shp:&nbsp;&nbsp;</em>A shapefile containing the deepest points for all U.S. lakes within HydroLakes.&nbsp; For more information on the deepest point see&nbsp;https://doi.org/10.5281/zenodo.4136754&nbsp; and Shen et al (2015).</p> <p><em>LakeExport.py</em>: Python code&nbsp;to extract reflectance values for U.S. lakes from Google Earth Engine.</p> <p><em>GEE_pull_functions.py: </em>Functions called within LakeExport.py</p> <p><em>01_LakeExtractor.Rmd:</em>&nbsp;An R Markdown file that takes the raw data from LakeExport.py and processes it for the final database.</p> <p><em>SceneMetadata.csv:</em>&nbsp;A file containing additional information such as scene cloud cover and sun angle for all Landsat scenes within the database.&nbsp; Can be joined to the final database using LandsatID.</p> <p><em>srCorrected_us_hydrolakes_dp_20200628:&nbsp;</em>The final LimnoSat-US database containing all cloud free observations of U.S. lakes from 1984-2020.&nbsp; Missing values for bands not shared between sensors (Aerosol and TIR2) are denoted by -99.&nbsp; dWL is the dominant wavelength calculated following Wang et al. (2015).&nbsp; pCount_dswe1 represents the number of high confidence water pixels within 120 meters of the deepest point.&nbsp; pCount_dswe3 represents the number of vegetated water pixels within 120 meters and can be used as a flag for potential reflectance noise.&nbsp; All reflectance values represent the median value of high confidence water pixels within 120 meters. The final database is provided in both as a .csv and .feather formats.&nbsp; It can be linked to SceneMetadata.cvs using LandsatID.&nbsp; All reflectance values are derived from USGS T1-SR Landsat scenes.</p>

opencc-by-4.0Oct 2020View details →
zenodo40/100

Reconstructed remote sensing land surface temperature data in North America in 2002-2018

<p>In order to more accurately study the change trend of land surface temperature in North America in recent years, we combined remote sensing and meteorological station data and used various restoration models to generate more accurate and more complete remote sensing land surface temperature data.&nbsp;Our data covered the North American continent from 2002 to&nbsp;2018, with a spatial resolution of 0.05&deg;&times;0.05&deg;.&nbsp;In order to facilitate the statistics of the data, we set the projection mode of the data as&nbsp;World_Cylindrical_Equal_Area. We collated the data from different time dimensions, including month, season and year.</p>

opencc-by-4.0Nov 2019View details →
dryad40/100

Data from: Shark movement strategies influence poaching risk and can guide enforcement decisions in a large, remote Marine Protected Area

<ol> <li>Large, remote marine protected areas (MPAs) containing both reef and pelagic habitats, have been shown to offer considerable refuge to populations of reef-associated sharks. Many large MPAs are, however, impacted by illegal fishing activity conducted by unlicensed vessels. While enforcement of these reserves is often expensive, it would likely benefit from the integration of ecological data on the mobile animals they are designed to protect. Consequently, shark populations in some protected areas continue to decline, as they remain a prime target for illegal fishers.</li> <li>To understand shark movements and their vulnerability to illegal fishing, three years of acoustic tracking data, from 101 reef-associated sharks, were analysed as movement networks to explore the predictability of movement patterns and identify key movement corridors within the British Indian Ocean Territory (BIOT) MPA. We examined how space use and connectivity overlap with spatially-explicit risk of illegal fishing, through data obtained from the management consultancy enforcing the MPA.</li> <li>Using individual-based models, the movement networks of two sympatric shark species were efficiently predicted with distance-decay functions (&gt;95% movements accurately predicted). Model outliers were used to highlight the locations with unexpectedly high movement rates where MPA enforcement patrols might most efficiently mitigate predator removal.</li> <li>Activity space estimates and network metrics illustrate that silvertip sharks were more dynamic, less resident and link larger components of the MPA than grey reef sharks. However, we show that this behaviour potentially enhances their exposure to illegal fishing activity.</li> <li> <i>Synthesis and applications. </i>Marine protected area (MPA) enforcement strategies are often limited by resources. The British Indian Ocean Territory MPA, one of the world's largest 'no take' MPAs, has a single patrol vessel to enforce 640,000 km<sup>2</sup> of open ocean, atoll and reef ecosystems. We argue that to optimise the patrol vessel search strategy and thus enhance their protective capacity, ecological data on the space use and movements of desirable species, such as large-bodied reef predators, must be incorporated into management plans. Here, we use electronic tracking data to evaluate how shark movement dynamics influence species mortality trajectories in exploited reef ecosystems. In doing so we discuss how network analyses of such data might be applied for protected area enforcement.</li> </ol>

opencc-zeroMay 2020View details →
zenodo40/100

Survey data for "Remote Sensing & GIS Training in Ecology and Conservation"

<p>This file provides the raw data of an online survey intended at gathering information regarding remote sensing (RS) and Geographical Information Systems (GIS) for conservation in academic education. The aim was to unfold best practices as well as gaps in teaching methods of remote sensing/GIS, and to help inform how these may be adapted and improved. A total of 73 people answered the survey, which was distributed through closed mailing lists of universities and conservation groups.</p>

opencc-zeroApr 2016View details →
zenodo40/100

MagicBathyNet: A Multimodal Remote Sensing Dataset for Bathymetry Prediction and Pixel-based Classification in Shallow Waters

<p><strong>The dataset</strong></p> <p>MagicBathyNet is a benchmark dataset made up of image patches of Sentinel-2, SPOT-6 and aerial imagery, bathymetry in raster format and seabed classes annotations. MagicBathyNet has been designed to be geographically well distributed. It&rsquo;s coverage includes two very different coastal areas (in terms of water column characteristics and bottom type): i) Agia Napa area in Cyprus, covering a wide range of typical Mediterranean waters and seabed types, and ii) Puck Lagoon area in Poland, representing in a great degree Baltic Sea waters and bottom.</p> <p>MagicBathyNet contains 3355 RGB co-registered triplets of Sentinel-2 (S2), SPOT-6, and aerial image patches, complemented by 1244 RGB co-registered S2 and SPOT-6 doublets, 3354 DSM (Digital Surface Model) raster patches for the aerial patches and 3396 DSM raster patches for S2 and SPOT-6. Additionally, it contains 533 annotated raster patches for seabed habitat and type, facilitating supervised pixel-based classification.&nbsp;Each patch covers 180x180m, represented by 18x18 pixels in S2 imagery, 30x30 pixels in SPOT-6 imagery and 720x720 pixels in airborne imagery.&nbsp;</p> <p>For the implementation code and pre-trained models visit our project page: <a href="https://www.magicbathy.eu/magicbathynet.html">https://www.magicbathy.eu/magicbathynet.html</a>&nbsp;</p> <p><strong>MagicBathyNet.zip </strong>file contains the original dataset presented in the respective paper.</p> <p><strong>MagicBathyNet_extension_for_Swin-BathyUNet.zip</strong> file is added in the new version to support the experiments and the results presented in "Agrafiotis, P., &amp; Demir, B. (2025). Deep learning-based bathymetry retrieval without in-situ depths using remote sensing imagery and SfM-MVS DSMs with data gaps. <em>ISPRS Journal of Photogrammetry and Remote Sensing</em>,&nbsp;<em>225</em>, 341-361. <a href="https://doi.org/10.1016/j.isprsjprs.2025.04.020">https://doi.org/10.1016/j.isprsjprs.2025.04.020</a> "</p> <p>&nbsp;</p> <p>&nbsp;</p> <p><strong>Citation</strong></p> <p>If you use the code in this repository or the dataset please cite our paper:</p> <p>P. Agrafiotis, L. Janowski, D. Skarlatos, and B. Demir,&nbsp;<a href="https://arxiv.org/abs/2405.15477" target="_blank" rel="noopener noreferrer">"MagicBathyNet: A Multimodal Remote Sensing Dataset for Bathymetry Prediction and Pixel-based Classification in Shallow Waters"</a>, arXiv:2405.15477, 2024.</p> <p>or&nbsp;</p> <p>P. Agrafiotis, Ł. Janowski, D. Skarlatos and B. Demir, "MAGICBATHYNET: A Multimodal Remote Sensing Dataset for Bathymetry Prediction and Pixel-Based Classification in Shallow Waters,"&nbsp;<em>IGARSS 2024 - 2024 IEEE International Geoscience and Remote Sensing Symposium</em>, Athens, Greece, 2024, pp. 249-253, doi: 10.1109/IGARSS53475.2024.10641355.</p> <p><strong>Folder structure</strong></p> <p>┗ 📂 magicbathynet/<br>&nbsp; ┣ 📂 agia_napa/<br>&nbsp; ┃ ┣ 📂 img/<br>&nbsp; ┃ ┃ ┣ 📂 aerial/<br>&nbsp; ┃ ┃ ┃ ┣ 📜 img_339.tif<br>&nbsp; ┃ ┃ ┃ ┣ 📜 ...<br>&nbsp; ┃ ┃ ┣ 📂 s2/<br>&nbsp; ┃ ┃ ┃ ┣ 📜 img_339.tif<br>&nbsp; ┃ ┃ ┃ ┣ 📜 ...<br>&nbsp; ┃ ┃ ┣ 📂 spot6/<br>&nbsp; ┃ ┃ ┃ ┣ 📜 img_339.tif<br>&nbsp; ┃ ┃ ┃ ┣ 📜 ...<br>&nbsp; ┃ ┣ 📂 depth/<br>&nbsp; ┃ ┃ ┣ 📂 aerial/<br>&nbsp; ┃ ┃ ┃ ┣ 📜 depth_339.tif<br>&nbsp; ┃ ┃ ┃ ┣ 📜 ...<br>&nbsp; ┃ ┃ ┣ 📂 s2/<br>&nbsp; ┃ ┃ ┃ ┣ 📜 depth_339.tif<br>&nbsp; ┃ ┃ ┃ ┣ 📜 ...<br>&nbsp; ┃ ┃ ┣ 📂 spot6/<br>&nbsp; ┃ ┃ ┃ ┣ 📜 depth_339.tif<br>&nbsp; ┃ ┃ ┃ ┣ 📜 ...<br>&nbsp; ┃ ┣ 📂 gts/<br>&nbsp; ┃ ┃ ┣ 📂 aerial/<br>&nbsp; ┃ ┃ ┃ ┣ 📜 gts_339.tif<br>&nbsp; ┃ ┃ ┃ ┣ 📜 ...<br>&nbsp; ┃ ┃ ┣ 📂 s2/<br>&nbsp; ┃ ┃ ┃ ┣ 📜 gts_339.tif<br>&nbsp; ┃ ┃ ┃ ┣ 📜 ...<br>&nbsp; ┃ ┃ ┣ 📂 spot6/<br>&nbsp; ┃ ┃ ┃ ┣ 📜 gts_339.tif<br>&nbsp; ┃ ┃ ┃ ┣ 📜 ...<br>&nbsp; ┃ ┣ 📜 [modality]_split_bathymetry.txt<br>&nbsp; ┃ ┣ 📜 [modality]_split_pixel_class.txt<br>&nbsp; ┃ ┣ 📜 norm_param_[modality]_an.txt<br>&nbsp; ┃<br>&nbsp; ┣ 📂 puck_lagoon/<br>&nbsp; ┃ ┣ 📂 img/<br>&nbsp; ┃ ┃ ┣ 📜 ...<br>&nbsp; ┃ ┣ 📂 depth/<br>&nbsp; ┃ ┃ ┣ 📜 ...<br>&nbsp; ┃ ┣ 📂 gts/<br>&nbsp; ┃ ┃ ┣ 📜 ...<br>&nbsp; ┃ ┣ 📜 [modality]_split_bathymetry.txt<br>&nbsp; ┃ ┣ 📜 [modality]_split_pixel_class.txt<br>&nbsp; ┃ ┣ 📜 norm_param_[modality]_pl.txt</p> <p>&nbsp;</p> <p><strong>Package for benchmarking MagicBathyNet dataset</strong></p> <p>Donwload the package for benchmarking MagicBathyNet dataset in learning-based bathymetry and pixel-based classification here:</p> <p><a href="https://github.com/pagraf/MagicBathyNet">https://github.com/pagraf/MagicBathyNet</a></p> <p>&nbsp;</p> <p><strong>Version history</strong></p> <p>v1.0.0 - First release</p> <p>&nbsp;</p> <p><strong>License</strong></p> <p>Dataset: Creative Commons Attribution Non Commercial 4.0 International</p> <p>Code: Attribution-NonCommercial-ShareAlike 4.0 International License</p> <p>Copyright (c) 2024 The MagicBathyNet Authors</p> <p>&nbsp;</p> <p><strong>Acknowledgments</strong></p> <p>This work was part of the project MagicBathy which is a research project funded by the European Commission for the period 2023-2025. It is funded under the HORIZON Europe MSCA Postdoctoral Fellowships - European Fellowships (GA 101063294).</p> <p>European Space Agency (ESA) is also acknowledged for providing the SPOT-6 images within its TPM programme in the frame of proposal PP0092443 and Airbus for being the provider of the original SPOT-6 images. The Dep. of Land and Surveys of Cyprus is acknowledged for providing the LiDAR reference data for Cyprus.</p>

opencc-by-nc-4.0May 2024View details →

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