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515 results for “swath”

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zenodo36/100

ELITE surface lognwave upwelling radiation: global 1km Swath 5-min SLUR - Aqua (2010.10-12)

<p>The <strong>E</strong>ssential therma<strong>L</strong> <strong>I</strong>nfrared remo<strong>T</strong>e s<strong>E</strong>nsing (<strong>ELITE</strong>) product suite currently has four types of products, including land surface temperature (LST: clear-sky and all-sky), emissivity (NBE: narrowband emissivity; BBE: broadband emissivity; and spectral emissivity), the component of surface radiation and energy budget (SLUR: surface longwave upwelling radiation; SLDR: surface longwave downward radiation SLDR; SLNR: surface longwave net radiation), and the component of Earth&rsquo;s radiation budget (OLR; outgoing longwave radiation; RSR: reflected solar radiation). The spatial-temporal resolutions of the ELITE products are mainly determined by the employed satellite data sources. For more information about ELITE products, please refer to the website (<a href="https://elite.bnu.edu.cn">https://elite.bnu.edu.cn</a>).</p> <p>This dataset is the ELITE global 1km instantaneous SLUR&nbsp;product ranging&nbsp;from 2000&nbsp;to 2022 (continuously updated). This dataset was generated from the Moderate Resolution Imaging Spectrometer (MODIS, Terra and Aqua) data using the algorithm developed by&nbsp;Cheng et al. (2016).&nbsp;</p> <p>This is the ELITE SLUR (Aqua)&nbsp;product in 2010.10-2010.12.&nbsp;&nbsp;Please&nbsp;<a href="https://zenodo.org/deposit/8255865"><strong><em>click here</em></strong></a>&nbsp;to download the ELITE SLNR (Aqua) product in 2010.01-2010.03&nbsp;and&nbsp;<a href="https://zenodo.org/deposit/8254000"><strong><em>click here</em></strong></a>&nbsp;to download the ELITE SLUR (Aqua) product in 2011.07-2011.09.</p> <p><strong>Dataset Characteristics:</strong></p> <ul> <li>Spatial Coverage: Global</li> <li>Temporal Coverage: 2010</li> <li>Spatial Resolution: 1 km</li> <li>Temporal Resolution: 5min/instantaneous</li> <li>Data Format: hdf</li> <li>Scale: 0.05</li> <li>Offset: -1000</li> </ul> <p><strong>Citation&nbsp;</strong>(Please cite these papers when using the data)<strong>:</strong></p> <ol> <li>Cheng, J., &amp; Liang, S. (2016). Global estimates for high-spatial-resolution clear-sky land surface upwelling longwave radiation from MODIS data.&nbsp;IEEE Transactions on Geoscience and Remote Sensing,&nbsp;<em>54</em>(7), 4115-4129.</li> </ol> <p>If you have any questions, please contact Prof. Jie Cheng (Jie_Cheng@bnu.edu.cn).</p> <ol> <li>Cheng J, Liang S. Global Estimates for High-Spatial-Resolution Clear-Sky Land Surface Upwelling Longwave Radiation From MODIS Data[J]. IEEE Transactions on Geoscience and Remote Sensing, 2016, 54(7): 4115-4129.</li> </ol> <p>If you have any questions, please contact Prof. Jie Cheng (Jie_Cheng@bnu.edu.cn).</p>

opencc-by-4.0Aug 2023View details →
zenodo36/100

ELITE surface lognwave upwelling radiation: global 1km Swath 5-min SLUR - Aqua (2010.07-09)

<p>The <strong>E</strong>ssential therma<strong>L</strong> <strong>I</strong>nfrared remo<strong>T</strong>e s<strong>E</strong>nsing (<strong>ELITE</strong>) product suite currently has four types of products, including land surface temperature (LST: clear-sky and all-sky), emissivity (NBE: narrowband emissivity; BBE: broadband emissivity; and spectral emissivity), the component of surface radiation and energy budget (SLUR: surface longwave upwelling radiation; SLDR: surface longwave downward radiation SLDR; SLNR: surface longwave net radiation), and the component of Earth&rsquo;s radiation budget (OLR; outgoing longwave radiation; RSR: reflected solar radiation). The spatial-temporal resolutions of the ELITE products are mainly determined by the employed satellite data sources. For more information about ELITE products, please refer to the website (<a href="https://elite.bnu.edu.cn">https://elite.bnu.edu.cn</a>).</p> <p>This dataset is the ELITE global 1km instantaneous SLUR&nbsp;product ranging&nbsp;from 2000&nbsp;to 2022 (continuously updated). This dataset was generated from the Moderate Resolution Imaging Spectrometer (MODIS, Terra and Aqua) data using the algorithm developed by&nbsp;Cheng et al. (2016).&nbsp;</p> <p>This is the ELITE SLUR (Aqua)&nbsp;product in 2010.07-2010.09.&nbsp;&nbsp;Please&nbsp;<a href="https://zenodo.org/deposit/8254000"><strong><em>click here</em></strong></a>&nbsp;to download the ELITE SLUR (Aqua) product in 2010.10-2010.12&nbsp;and&nbsp;<a href="https://zenodo.org/deposit/8252086"><strong><em>click here</em></strong></a>&nbsp;to download the ELITE SLUR (Aqua) product in 2011.04-2011.06.</p> <p><strong>Dataset Characteristics:</strong></p> <ul> <li>Spatial Coverage: Global</li> <li>Temporal Coverage: 2010</li> <li>Spatial Resolution: 1 km</li> <li>Temporal Resolution: 5min/instantaneous</li> <li>Data Format: hdf</li> <li>Scale: 0.05</li> <li>Offset: -1000</li> </ul> <p><strong>Citation&nbsp;</strong>(Please cite these papers when using the data)<strong>:</strong></p> <ol> <li>Cheng, J., &amp; Liang, S. (2016). Global estimates for high-spatial-resolution clear-sky land surface upwelling longwave radiation from MODIS data.&nbsp;IEEE Transactions on Geoscience and Remote Sensing,&nbsp;<em>54</em>(7), 4115-4129.</li> </ol> <p>If you have any questions, please contact Prof. Jie Cheng (Jie_Cheng@bnu.edu.cn).</p> <ol> <li>Cheng J, Liang S. Global Estimates for High-Spatial-Resolution Clear-Sky Land Surface Upwelling Longwave Radiation From MODIS Data[J]. IEEE Transactions on Geoscience and Remote Sensing, 2016, 54(7): 4115-4129.</li> </ol> <p>If you have any questions, please contact Prof. Jie Cheng (Jie_Cheng@bnu.edu.cn).</p>

opencc-by-4.0Aug 2023View details →
zenodo36/100

ELITE surface lognwave upwelling radiation: global 1km Swath 5-min SLUR - Aqua (2010.04-06)

<p>The <strong>E</strong>ssential therma<strong>L</strong> <strong>I</strong>nfrared remo<strong>T</strong>e s<strong>E</strong>nsing (<strong>ELITE</strong>) product suite currently has four types of products, including land surface temperature (LST: clear-sky and all-sky), emissivity (NBE: narrowband emissivity; BBE: broadband emissivity; and spectral emissivity), the component of surface radiation and energy budget (SLUR: surface longwave upwelling radiation; SLDR: surface longwave downward radiation SLDR; SLNR: surface longwave net radiation), and the component of Earth&rsquo;s radiation budget (OLR; outgoing longwave radiation; RSR: reflected solar radiation). The spatial-temporal resolutions of the ELITE products are mainly determined by the employed satellite data sources. For more information about ELITE products, please refer to the website (<a href="https://elite.bnu.edu.cn">https://elite.bnu.edu.cn</a>).</p> <p>This dataset is the ELITE global 1km instantaneous SLUR&nbsp;product ranging&nbsp;from 2000&nbsp;to 2022 (continuously updated). This dataset was generated from the Moderate Resolution Imaging Spectrometer (MODIS, Terra and Aqua) data using the algorithm developed by&nbsp; Cheng et al. (2016).&nbsp;</p> <p>This is the ELITE SLUR (Aqua)&nbsp;product in 2010.04-2010.06.&nbsp;Please&nbsp;<a href="https://zenodo.org/deposit/8252082"><strong><em>click here</em></strong></a>&nbsp;to download the ELITE SLUR (Aqua) product in 2010.01-2010.03&nbsp;and&nbsp;<a href="https://zenodo.org/deposit/8254002"><strong><em>click here</em></strong></a>&nbsp;to download the ELITE SLUR Aqua) product in 2010.07-2010.09.</p> <p><strong>Dataset Characteristics:</strong></p> <ul> <li>Spatial Coverage: Global</li> <li>Temporal Coverage: 2010</li> <li>Spatial Resolution: 1 km</li> <li>Temporal Resolution: 5min/instantaneous</li> <li>Data Format: hdf</li> <li>Scale: 0.05</li> <li>Offset: -1000</li> </ul> <p><strong>Citation&nbsp;</strong>(Please cite these papers when using the data)<strong>:</strong></p> <ol> <li>Cheng, J., &amp; Liang, S. (2016). Global estimates for high-spatial-resolution clear-sky land surface upwelling longwave radiation from MODIS data.&nbsp;IEEE Transactions on Geoscience and Remote Sensing,&nbsp;<em>54</em>(7), 4115-4129.</li> </ol> <p>If you have any questions, please contact Prof. Jie Cheng (Jie_Cheng@bnu.edu.cn).</p> <p><strong>Dataset Characteristics:</strong></p> <ul> <li>Spatial Coverage: Global</li> <li>Temporal Coverage: 2010</li> <li>Spatial Resolution: 1 km</li> <li>Temporal Resolution: 5-min</li> <li>Data Format: hdf</li> <li>Scale: 0.05</li> <li>Offset: -1000</li> </ul> <p><strong>Citation&nbsp;</strong>(Please cite these papers when using the data)<strong>:</strong></p> <ol> <li>Cheng J, Liang S. Global Estimates for High-Spatial-Resolution Clear-Sky Land Surface Upwelling Longwave Radiation From MODIS Data[J]. IEEE Transactions on Geoscience and Remote Sensing, 2016, 54(7): 4115-4129.</li> </ol> <p>If you have any questions, please contact Prof. Jie Cheng (Jie_Cheng@bnu.edu.cn).</p>

opencc-by-4.0Aug 2023View details →
zenodo36/100

ELITE surface longwave upwelling radiation: global 1km Swath 5-min SLUR - Aqua (2010.01-03)

<p>The <strong>E</strong>ssential therma<strong>L</strong> <strong>I</strong>nfrared remo<strong>T</strong>e s<strong>E</strong>nsing (<strong>ELITE</strong>) product suite currently has four types of products, including land surface temperature (LST: clear-sky and all-sky), emissivity (NBE: narrowband emissivity; BBE: broadband emissivity; and spectral emissivity), the component of surface radiation and energy budget (SLUR: surface longwave upwelling radiation; SLDR: surface longwave downward radiation SLDR; SLNR: surface longwave net radiation), and the component of Earth&rsquo;s radiation budget (OLR; outgoing longwave radiation; RSR: reflected solar radiation). The spatial-temporal resolutions of the ELITE products are mainly determined by the employed satellite data sources. For more information about ELITE products, please refer to the website (<a href="https://elite.bnu.edu.cn">https://elite.bnu.edu.cn</a>).</p> <p>This dataset is the ELITE global 1km instantaneous SLUR&nbsp;product ranging&nbsp;from 2000&nbsp;to 2022 (continuously updated). This dataset was generated from the Moderate Resolution Imaging Spectrometer (MODIS, Terra and Aqua) data using the algorithm developed by&nbsp;Cheng et al. (2016).&nbsp;</p> <p>This is the ELITE SLUR (Aqua)&nbsp;product in 2010.01-2010.03.&nbsp;Please&nbsp;<a href="https://zenodo.org/deposit/8237637"><strong><em>click here</em></strong></a>&nbsp;to download the ELITE SLDR (Aqua) product in 2009.10-2009.12&nbsp;and&nbsp;<a href="https://zenodo.org/deposit/8252086"><strong><em>click here</em></strong></a>&nbsp;to download the ELITE SLUR (Aqua) product in 2010.04-2010.06.</p> <p><strong>Dataset Characteristics:</strong></p> <ul> <li>Spatial Coverage: Global</li> <li>Temporal Coverage: 2010</li> <li>Spatial Resolution: 1 km</li> <li>Temporal Resolution: 5min/instantaneous</li> <li>Data Format: hdf</li> <li>Scale: 0.05</li> <li>Offset: -1000</li> </ul> <p><strong>Citation&nbsp;</strong>(Please cite these papers when using the data)<strong>:</strong></p> <ol> <li>Cheng, J., &amp; Liang, S. (2016). Global estimates for high-spatial-resolution clear-sky land surface upwelling longwave radiation from MODIS data.&nbsp;IEEE Transactions on Geoscience and Remote Sensing,&nbsp;<em>54</em>(7), 4115-4129.</li> </ol> <p>If you have any questions, please contact Prof. Jie Cheng (Jie_Cheng@bnu.edu.cn).</p>

opencc-by-4.0Aug 2023View details →
zenodo36/100

ELITE surface longwave upwelling radiation: global 1km Swath 5-min SLUR - Terra (2010.10-12)

<p>The <strong>E</strong>ssential therma<strong>L</strong> <strong>I</strong>nfrared remo<strong>T</strong>e s<strong>E</strong>nsing (<strong>ELITE</strong>) product suite currently has four types of products, including land surface temperature (LST: clear-sky and all-sky), emissivity (NBE: narrowband emissivity; BBE: broadband emissivity; and spectral emissivity), the component of surface radiation and energy budget (SLUR: surface longwave upwelling radiation; SLDR: surface longwave downward radiation SLDR; SLNR: surface longwave net radiation), and the component of Earth&rsquo;s radiation budget (OLR; outgoing longwave radiation; RSR: reflected solar radiation). The spatial-temporal resolutions of the ELITE products are mainly determined by the employed satellite data sources. For more information about ELITE products, please refer to the website (<a href="https://elite.bnu.edu.cn">https://elite.bnu.edu.cn</a>).</p> <p>This dataset is the ELITE global 1km instantaneous SLUR&nbsp;product ranging&nbsp;from 2000&nbsp;to 2022 (continuously updated). This dataset was generated from the Moderate Resolution Imaging Spectrometer (MODIS, Terra and Aqua) data using the algorithm developed by&nbsp; Cheng et al. (2016).&nbsp;</p> <p>This is the ELITE SLUR (Terra)&nbsp;product in 2010.10-2010.12.&nbsp;Please&nbsp;<a href="https://zenodo.org/record/8251659"><strong><em>click here</em></strong></a>&nbsp;to download the ELITE SLUR (Terra) product in 2010.07-2010.09&nbsp;and&nbsp;<a href="https://zenodo.org/record/7281765"><strong><em>click here</em></strong></a>&nbsp;to download the ELITE SLUR (Terra) product in 2011.01-2011.03.</p> <p><strong>Dataset Characteristics:</strong></p> <ul> <li>Spatial Coverage: Global</li> <li>Temporal Coverage: 2010</li> <li>Spatial Resolution: 1 km</li> <li>Temporal Resolution: 5min/instantaneous</li> <li>Data Format: hdf</li> <li>Scale: 0.05</li> <li>Offset: -1000</li> </ul> <p><strong>Citation&nbsp;</strong>(Please cite these papers when using the data)<strong>:</strong></p> <ol> <li>Cheng, J., &amp; Liang, S. (2016). Global estimates for high-spatial-resolution clear-sky land surface upwelling longwave radiation from MODIS data.&nbsp;IEEE Transactions on Geoscience and Remote Sensing,&nbsp;<em>54</em>(7), 4115-4129.</li> </ol> <p>If you have any questions, please contact Prof. Jie Cheng (Jie_Cheng@bnu.edu.cn).</p>

opencc-by-4.0Aug 2023View details →
zenodo36/100

ELITE surface longwave upwelling radiation: global 1km Swath 5-min SLUR - Terra (2010.01-03)

<p>The <strong>E</strong>ssential therma<strong>L</strong> <strong>I</strong>nfrared remo<strong>T</strong>e s<strong>E</strong>nsing (<strong>ELITE</strong>) product suite currently has four types of products, including land surface temperature (LST: clear-sky and all-sky), emissivity (NBE: narrowband emissivity; BBE: broadband emissivity; and spectral emissivity), the component of surface radiation and energy budget (SLUR: surface longwave upwelling radiation; SLDR: surface longwave downward radiation SLDR; SLNR: surface longwave net radiation), and the component of Earth&rsquo;s radiation budget (OLR; outgoing longwave radiation; RSR: reflected solar radiation). The spatial-temporal resolutions of the ELITE products are mainly determined by the employed satellite data sources. For more information about ELITE products, please refer to the website (<a href="https://elite.bnu.edu.cn">https://elite.bnu.edu.cn</a>).</p> <p>This dataset is the ELITE global 1km instantaneous SLUR&nbsp;product ranging&nbsp;from 2000&nbsp;to 2022 (continuously updated). This dataset was generated from the Moderate Resolution Imaging Spectrometer (MODIS, Terra and Aqua) data using the algorithm developed by&nbsp; Cheng et al. (2016).&nbsp;</p> <p>This is the ELITE SLUR (Terra)&nbsp;product in 2010.01-2010.03.&nbsp;Please&nbsp;<a href="https://www.zenodo.org/record/8251664"><strong><em>click here</em></strong></a>&nbsp;to download the ELITE SLUR (Terra) product in 2009.10-2009.12&nbsp;and&nbsp;<a href="https://zenodo.org/record/7281765"><strong><em>click here</em></strong></a>&nbsp;to download the ELITE SLUR (Terra) product in 2010.04-2010.06.</p> <p><strong>Dataset Characteristics:</strong></p> <ul> <li>Spatial Coverage: Global</li> <li>Temporal Coverage: 2010</li> <li>Spatial Resolution: 1 km</li> <li>Temporal Resolution: 5min/instantaneous</li> <li>Data Format: hdf</li> <li>Scale: 0.05</li> <li>Offset: -1000</li> </ul> <p><strong>Citation&nbsp;</strong>(Please cite these papers when using the data)<strong>:</strong></p> <ol> <li>Cheng, J., &amp; Liang, S. (2016). Global estimates for high-spatial-resolution clear-sky land surface upwelling longwave radiation from MODIS data.&nbsp;IEEE Transactions on Geoscience and Remote Sensing,&nbsp;<em>54</em>(7), 4115-4129.</li> </ol> <p>If you have any questions, please contact Prof. Jie Cheng (Jie_Cheng@bnu.edu.cn).</p>

opencc-by-4.0Aug 2023View details →
zenodo36/100

ELITE surface longwave upwelling radiation: global 1km Swath 5-min SLUR - Terra (2010.07-09)

<p>The <strong>E</strong>ssential therma<strong>L</strong> <strong>I</strong>nfrared remo<strong>T</strong>e s<strong>E</strong>nsing (<strong>ELITE</strong>) product suite currently has four types of products, including land surface temperature (LST: clear-sky and all-sky), emissivity (NBE: narrowband emissivity; BBE: broadband emissivity; and spectral emissivity), the component of surface radiation and energy budget (SLUR: surface longwave upwelling radiation; SLDR: surface longwave downward radiation SLDR; SLNR: surface longwave net radiation), and the component of Earth&rsquo;s radiation budget (OLR; outgoing longwave radiation; RSR: reflected solar radiation). The spatial-temporal resolutions of the ELITE products are mainly determined by the employed satellite data sources. For more information about ELITE products, please refer to the website (<a href="https://elite.bnu.edu.cn">https://elite.bnu.edu.cn</a>).</p> <p>This dataset is the ELITE global 1km instantaneous SLUR&nbsp;product ranging&nbsp;from 2000&nbsp;to 2022 (continuously updated). This dataset was generated from the Moderate Resolution Imaging Spectrometer (MODIS, Terra and Aqua) data using the algorithm developed by&nbsp; Cheng et al. (2016).&nbsp;</p> <p>This is the ELITE SLUR (Terra)&nbsp;product in 2010.07-2010.09.&nbsp;Please&nbsp;<a href="https://zenodo.org/record/8251664"><strong><em>click here</em></strong></a>&nbsp;to download the ELITE SLUR (Terra) product in 2010.04-2010.06&nbsp;and&nbsp;<a href="https://www.zenodo.org/record/8251880"><strong><em>click here</em></strong></a>&nbsp;to download the ELITE SLUR (Terra) product in 2010.10-2010.12.</p> <p><strong>Dataset Characteristics:</strong></p> <ul> <li>Spatial Coverage: Global</li> <li>Temporal Coverage: 2010</li> <li>Spatial Resolution: 1 km</li> <li>Temporal Resolution: 5min/instantaneous</li> <li>Data Format: hdf</li> <li>Scale: 0.05</li> <li>Offset: -1000</li> </ul> <p><strong>Citation&nbsp;</strong>(Please cite these papers when using the data)<strong>:</strong></p> <ol> <li>Cheng, J., &amp; Liang, S. (2016). Global estimates for high-spatial-resolution clear-sky land surface upwelling longwave radiation from MODIS data.&nbsp;IEEE Transactions on Geoscience and Remote Sensing,&nbsp;<em>54</em>(7), 4115-4129.</li> </ol> <p>If you have any questions, please contact Prof. Jie Cheng (Jie_Cheng@bnu.edu.cn).</p>

opencc-by-4.0Aug 2023View details →
zenodo36/100

ELITE surface longwave upwelling radiation: global 1km Swath 5-min SLUR - Terra (2010.04-06)

<p>The <strong>E</strong>ssential therma<strong>L</strong> <strong>I</strong>nfrared remo<strong>T</strong>e s<strong>E</strong>nsing (<strong>ELITE</strong>) product suite currently has four types of products, including land surface temperature (LST: clear-sky and all-sky), emissivity (NBE: narrowband emissivity; BBE: broadband emissivity; and spectral emissivity), the component of surface radiation and energy budget (SLUR: surface longwave upwelling radiation; SLDR: surface longwave downward radiation SLDR; SLNR: surface longwave net radiation), and the component of Earth&rsquo;s radiation budget (OLR; outgoing longwave radiation; RSR: reflected solar radiation). The spatial-temporal resolutions of the ELITE products are mainly determined by the employed satellite data sources. For more information about ELITE products, please refer to the website (<a href="https://elite.bnu.edu.cn">https://elite.bnu.edu.cn</a>).</p> <p>This dataset is the ELITE global 1km instantaneous SLUR&nbsp;product ranging&nbsp;from 2000&nbsp;to 2022 (continuously updated). This dataset was generated from the Moderate Resolution Imaging Spectrometer (MODIS, Terra and Aqua) data using the algorithm developed by&nbsp; Cheng et al. (2016).&nbsp;</p> <p>This is the ELITE SLUR (Terra)&nbsp;product in 2010.04-2010.06.&nbsp;Please&nbsp;<a href="https://www.zenodo.org/record/8251604"><strong><em>click here</em></strong></a>&nbsp;to download the ELITE SLUR (Terra) product in 2010.01-2010.03&nbsp;and&nbsp;<a href="https://www.zenodo.org/record/8251659"><strong><em>click here</em></strong></a>&nbsp;to download the ELITE SLUR (Terra) product in 2010.07-2010.09.</p> <p><strong>Dataset Characteristics:</strong></p> <ul> <li>Spatial Coverage: Global</li> <li>Temporal Coverage: 2010</li> <li>Spatial Resolution: 1 km</li> <li>Temporal Resolution: 5min/instantaneous</li> <li>Data Format: hdf</li> <li>Scale: 0.05</li> <li>Offset: -1000</li> </ul> <p><strong>Citation&nbsp;</strong>(Please cite these papers when using the data)<strong>:</strong></p> <ol> <li>Cheng, J., &amp; Liang, S. (2016). Global estimates for high-spatial-resolution clear-sky land surface upwelling longwave radiation from MODIS data.&nbsp;IEEE Transactions on Geoscience and Remote Sensing,&nbsp;<em>54</em>(7), 4115-4129.</li> </ol> <p>If you have any questions, please contact Prof. Jie Cheng (Jie_Cheng@bnu.edu.cn).</p>

opencc-by-4.0Aug 2023View details →
zenodo32/100

Swath Bathymetry Pitman fracture zone

<p>Swath bathymetry for R.V. Ewing 89</p>

opencc-zeroOct 2013View details →
zenodo32/100

Subspecies and Distribution. A. p. palliata Gray, 1849 — NE Guatemala (Rio Motagua, and possibly along the coast a short distance to Cabo de Tres Puntas, where it meets the distribution of the Central American Black Howler, A. pigra), E to E Costa Rica or W Panama; it is not found in El Salvador, although it may have occurred there in the past. A. p. aequatorialis Festa, 1903 — from the S distributional limits of the nominate subspecies palliata (either in E Costa Rica or W Panama) through the Serrania del Darién into W Colombia (N through basins of the rios Sint and Atrato to the Caribbean coast, and S through the Serrania del Baudo and the foothills, lowlands, and lower montane areas W of the Andes to the Pacific coast), W Ecuador, and NW Peru (extreme N of Tumbes Department). A. p. coibensis Thomas, 1902 — SW Panama (Coiba and Jicaron Is). A. p. mexicana Merriam, 1902 — S & SE Mexico (states of Veracruz, Tabasco, Campeche, Oaxaca, and N Chiapas) and Guatemala, in a swathe skirting the S of the distribution of the Central American Black Howler. A. p. trabeata Lawrence, 1933 — SW Panama (Azuero Peninsula). in Atelidae

Subspecies and Distribution. A. p. palliata Gray, 1849 — NE Guatemala (Rio Motagua, and possibly along the coast a short distance to Cabo de Tres Puntas, where it meets the distribution of the Central American Black Howler, A. pigra), E to E Costa Rica or W Panama; it is not found in El Salvador, although it may have occurred there in the past. A. p. aequatorialis Festa, 1903 — from the S distributional limits of the nominate subspecies palliata (either in E Costa Rica or W Panama) through the Serrania del Darién into W Colombia (N through basins of the rios Sint and Atrato to the Caribbean coast, and S through the Serrania del Baudo and the foothills, lowlands, and lower montane areas W of the Andes to the Pacific coast), W Ecuador, and NW Peru (extreme N of Tumbes Department). A. p. coibensis Thomas, 1902 — SW Panama (Coiba and Jicaron Is). A. p. mexicana Merriam, 1902 — S &amp; SE Mexico (states of Veracruz, Tabasco, Campeche, Oaxaca, and N Chiapas) and Guatemala, in a swathe skirting the S of the distribution of the Central American Black Howler. A. p. trabeata Lawrence, 1933 — SW Panama (Azuero Peninsula).

opennotspecifiedMar 2013View details →
zenodo32/100

Data for SWATH-based Quantitative Proteomic Analysis of Morus alba L. Leaf under Ultraviolet-B radiation and Dark Treatment

<p><em>Morus alba (M. alba) </em>have been used in traditional Chinese medicine. Since, previous studies indicated that the accumulation of several secondary metabolites was significantly induced by UV-B radiation with dark treatment. To investigate the response of <em>Morus alba</em> leaf to UV-B radiation and UV-B radiation followed by dark incubation (UVD), SWATH-based quantitative proteomic analysis was performed on <em>Morus alba</em> leaf of control, UV-B radiation and UV-B radiation then dark incubation. A total of 716 proteins were identified and quantified.</p>

opencc-by-4.0Feb 2022View details →
zenodo32/100

Preliminary Results of Marine Gravity Anomaly and Bathymetry from SWOT Wide-Swath altimeter data

<p><span>We explore the potential of Ka-band radar interferometry (KaRIn) data from the SWOT mission for marine gravity and bathymetry applications. Our evaluation includes determining the deflection of vertical (DOV) using the least squares collocation (LSC) method, recovering gravity anomalies with the inverse Vening-Meinesz (IVM) approach, and predicting bathymetry through the gravity-geological method (GGM). SWOT-derived gravity anomalies in the study area, located between 20&ordm;N - 30&ordm;N and 135&ordm;E - 145&ordm;E, lies at the convergence of the Pacific and Eurasian tectonic plates. &nbsp;KaRIn data (only seven months) recovered gravity anomalies with an accuracy of 2.37 mGal, which is better than current models.</span></p> <p><span>The details of the method are discussed in a manuscript submitted to GRL.</span></p> <p>&nbsp;</p>

opencc-by-4.0Jun 2024View details →
zenodo32/100

ELITE surface longwave downward radiation: global 1km Swath 5-min SLDR - Aqua (2010.07-09)

<p>The <strong>E</strong>ssential therma<strong>L</strong> <strong>I</strong>nfrared remo<strong>T</strong>e s<strong>E</strong>nsing (<strong>ELITE</strong>) product suite currently has four types of products, including land surface temperature (LST: clear-sky and all-sky), emissivity (NBE: narrowband emissivity; BBE: broadband emissivity; and spectral emissivity), the component of surface radiation and energy budget (SLUR: surface longwave upwelling radiation; SLDR: surface longwave downward radiation SLDR; SLNR: surface longwave net radiation), and the component of Earth&rsquo;s radiation budget (OLR; outgoing longwave radiation; RSR: reflected solar radiation). The spatial-temporal resolutions of the ELITE products are mainly determined by the employed satellite data sources. For more information about ELITE products, please refer to the website (<a href="https://elite.bnu.edu.cn">https://elite.bnu.edu.cn</a>).</p> <p>This dataset is the ELITE global 1km instantaneous SLDR&nbsp;product ranging&nbsp;from 2000&nbsp;to 2022 (continuously updated). This dataset was generated from the Moderate Resolution Imaging Spectrometer (MODIS, Terra and Aqua) data using the algorithm developed by&nbsp;Cheng et al. (2017) and Yang and Cheng. (2020).</p> <p>This is the ELITE SLDR (Aqua)&nbsp;product in 2010.07-2010.09.&nbsp;Please&nbsp;<a href="https://zenodo.org/record/8237625"><strong><em>click here</em></strong></a>&nbsp;to download the ELITE SLDR (Aqua) product in 2010.04-2010.06&nbsp;and&nbsp;<a href="https://zenodo.org/record/8237637"><strong><em>click here</em></strong></a>&nbsp;to download the ELITE SLDR (Aqua) product in 2010.10-2010.12.</p> <p><strong>Dataset Characteristics:</strong></p> <ul> <li>Spatial Coverage: Global</li> <li>Temporal Coverage: 2010</li> <li>Spatial Resolution: 1 km</li> <li>Temporal Resolution: 5min/instantaneous</li> <li>Data Format: hdf</li> <li>Scale: 0.05</li> <li>Offset: -1000</li> </ul> <p><strong>Citation&nbsp;</strong>(Please cite these papers when using the data)<strong>:</strong></p> <ol> <li>Cheng J, Liang S, Wang W, et al. An efficient hybrid method for estimating clear‐sky surface downward longwave radiation from MODIS data. Journal of Geophysical Research: Atmospheres, 2017, 122(5): 2616-2630.</li> <li>Yang, F., &amp; Cheng, J. (2020). A framework for estimating cloudy sky surface downward longwave radiation from the derived active and passive cloud property parameters. Remote Sensing of Environment, 248, 111972.</li> </ol> <p>If you have any questions, please contact Prof. Jie Cheng (Jie_Cheng@bnu.edu.cn).</p>

opencc-by-4.0Aug 2023View details →
zenodo32/100

ELITE surface longwave downward radiation: global 1km Swath 5-min SLDR - Terra (2010.10-12)

<p>The <strong>E</strong>ssential therma<strong>L</strong> <strong>I</strong>nfrared remo<strong>T</strong>e s<strong>E</strong>nsing (<strong>ELITE</strong>) product suite currently has four types of products, including land surface temperature (LST: clear-sky and all-sky), emissivity (NBE: narrowband emissivity; BBE: broadband emissivity; and spectral emissivity), the component of surface radiation and energy budget (SLUR: surface longwave upwelling radiation; SLDR: surface longwave downward radiation SLDR; SLNR: surface longwave net radiation), and the component of Earth&rsquo;s radiation budget (OLR; outgoing longwave radiation; RSR: reflected solar radiation). The spatial-temporal resolutions of the ELITE products are mainly determined by the employed satellite data sources. For more information about ELITE products, please refer to the website (<a href="https://elite.bnu.edu.cn">https://elite.bnu.edu.cn</a>).</p> <p>This dataset is the ELITE global 1km instantaneous SLDR&nbsp;product ranging&nbsp;from 2000&nbsp;to 2022 (continuously updated). This dataset was generated from the Moderate Resolution Imaging Spectrometer (MODIS, Terra and Aqua) data using the algorithm developed by&nbsp;Cheng et al. (2017) and Yang and Cheng. (2020).</p> <p>This is the ELITE SLDR (Terra)&nbsp;product in 2010.10-2010.12. Please&nbsp;<a href="https://zenodo.org/record/8241646"><strong><em>click here</em></strong></a>&nbsp;to download the ELITE SLDR (Terra) product in 2010.07-2010.09&nbsp;and&nbsp;<a href="https://zenodo.org/deposit/8237629"><strong><em>click here</em></strong></a>&nbsp;to download the ELITE SLDR (Terra) product in 2011.01-2011.03.</p> <p><strong>Dataset Characteristics:</strong></p> <ul> <li>Spatial Coverage: Global</li> <li>Temporal Coverage: 2010</li> <li>Spatial Resolution: 1 km</li> <li>Temporal Resolution: 5min/instantaneous</li> <li>Data Format: hdf</li> <li>Scale: 0.05</li> <li>Offset: -1000</li> </ul> <p><strong>Citation&nbsp;</strong>(Please cite these papers when using the data)<strong>:</strong></p> <ol> <li>Cheng J, Liang S, Wang W, et al. An efficient hybrid method for estimating clear‐sky surface downward longwave radiation from MODIS data. Journal of Geophysical Research: Atmospheres, 2017, 122(5): 2616-2630.</li> <li>Yang, F., &amp; Cheng, J. (2020). A framework for estimating cloudy sky surface downward longwave radiation from the derived active and passive cloud property parameters. Remote Sensing of Environment, 248, 111972.</li> </ol> <p>If you have any questions, please contact Prof. Jie Cheng (Jie_Cheng@bnu.edu.cn).</p>

opencc-by-4.0Aug 2023View details →
zenodo32/100

ELITE surface longwave downward radiation: global 1km Swath 5-min SLDR - Terra (2010.07-09)

<p>The <strong>E</strong>ssential therma<strong>L</strong> <strong>I</strong>nfrared remo<strong>T</strong>e s<strong>E</strong>nsing (<strong>ELITE</strong>) product suite currently has four types of products, including land surface temperature (LST: clear-sky and all-sky), emissivity (NBE: narrowband emissivity; BBE: broadband emissivity; and spectral emissivity), the component of surface radiation and energy budget (SLUR: surface longwave upwelling radiation; SLDR: surface longwave downward radiation SLDR; SLNR: surface longwave net radiation), and the component of Earth&rsquo;s radiation budget (OLR; outgoing longwave radiation; RSR: reflected solar radiation). The spatial-temporal resolutions of the ELITE products are mainly determined by the employed satellite data sources. For more information about ELITE products, please refer to the website (<a href="https://elite.bnu.edu.cn">https://elite.bnu.edu.cn</a>).</p> <p>This dataset is the ELITE global 1km instantaneous SLDR&nbsp;product ranging&nbsp;from 2000&nbsp;to 2022 (continuously updated). This dataset was generated from the Moderate Resolution Imaging Spectrometer (MODIS, Terra and Aqua) data using the algorithm developed by&nbsp;Cheng et al. (2017) and Yang and Cheng. (2020).</p> <p>This is the ELITE SLDR (Terra)&nbsp;product in 2010.07-2010.09.&nbsp;Please&nbsp;<a href="https://zenodo.org/record/8241462"><strong><em>click here</em></strong></a>&nbsp;to download the ELITE SLDR (Terra) product in 2010.04-2010.06&nbsp;and&nbsp;<a href="https://www.zenodo.org/record/8241651"><strong><em>click here</em></strong></a>&nbsp;to download the ELITE SLDR (Terra) product in 2010.10-2010.12.</p> <p><strong>Dataset Characteristics:</strong></p> <ul> <li>Spatial Coverage: Global</li> <li>Temporal Coverage: 2010</li> <li>Spatial Resolution: 1 km</li> <li>Temporal Resolution: 5min/instantaneous</li> <li>Data Format: hdf</li> <li>Scale: 0.05</li> <li>Offset: -1000</li> </ul> <p><strong>Citation&nbsp;</strong>(Please cite these papers when using the data)<strong>:</strong></p> <ol> <li>Cheng J, Liang S, Wang W, et al. An efficient hybrid method for estimating clear‐sky surface downward longwave radiation from MODIS data. Journal of Geophysical Research: Atmospheres, 2017, 122(5): 2616-2630.</li> <li>Yang, F., &amp; Cheng, J. (2020). A framework for estimating cloudy sky surface downward longwave radiation from the derived active and passive cloud property parameters. Remote Sensing of Environment, 248, 111972.</li> </ol> <p>If you have any questions, please contact Prof. Jie Cheng (Jie_Cheng@bnu.edu.cn).</p>

opencc-by-4.0Aug 2023View details →
zenodo32/100

ELITE surface longwave net radiation: global 1km Swath 5-min SLNR - Aqua (2010.07-09)

<p>The <strong>E</strong>ssential therma<strong>L</strong> <strong>I</strong>nfrared remo<strong>T</strong>e s<strong>E</strong>nsing (<strong>ELITE</strong>) product suite currently has four types of products, including land surface temperature (LST: clear-sky and all-sky), emissivity (NBE: narrowband emissivity; BBE: broadband emissivity; and spectral emissivity), the component of surface radiation and energy budget (SLUR: surface longwave upwelling radiation; SLDR: surface longwave downward radiation SLDR; SLNR: surface longwave net radiation), and the component of Earth&rsquo;s radiation budget (OLR; outgoing longwave radiation; RSR: reflected solar radiation). The spatial-temporal resolutions of the ELITE products are mainly determined by the employed satellite data sources. For more information about ELITE products, please refer to the website (<a href="https://elite.bnu.edu.cn">https://elite.bnu.edu.cn</a>).</p> <p>This dataset is the ELITE global 1km instantaneous SLNR&nbsp;product ranging&nbsp;from 2000&nbsp;to 2022 (continuously updated). This dataset was generated from the Moderate Resolution Imaging Spectrometer (MODIS, Terra and Aqua) data using the algorithm developed by&nbsp;Cheng et al. (2016), Cheng et al. (2017), and Yang and Cheng. (2020).&nbsp;</p> <p>This is the ELITE SLNR (Aqua)&nbsp;product in 2010.07-2010.09.&nbsp;Please&nbsp;<a href="https://zenodo.org/record/8240689"><strong><em>click here</em></strong></a>&nbsp;to download the ELITE SLNR (Aqua) product in 2010.04-2010.06&nbsp;and&nbsp;<a href="https://zenodo.org/record/8243322"><strong><em>click here</em></strong></a>&nbsp;to download the ELITE SLNR (Aqua) product in 2010.10-2010.12.</p> <p><strong>Dataset Characteristics:</strong></p> <ul> <li>Spatial Coverage: Global</li> <li>Temporal Coverage: 2010</li> <li>Spatial Resolution: 1 km</li> <li>Temporal Resolution: 5min/instantaneous</li> <li>Data Format: hdf</li> <li>Scale: 0.05</li> <li>Offset: -1000</li> </ul> <p><strong>Citation&nbsp;</strong>(Please cite these papers when using the data)<strong>:</strong></p> <ol> <li>Cheng, J., &amp; Liang, S. (2016). Global estimates for high-spatial-resolution clear-sky land surface upwelling longwave radiation from MODIS data.&nbsp;IEEE Transactions on Geoscience and Remote Sensing,&nbsp;<em>54</em>(7), 4115-4129.</li> <li>Cheng J, Liang S, Wang W, et al. An efficient hybrid method for estimating clear‐sky surface downward longwave radiation from MODIS data. Journal of Geophysical Research: Atmospheres, 2017, 122(5): 2616-2630.</li> <li>Yang, F., &amp; Cheng, J. (2020). A framework for estimating cloudy sky surface downward longwave radiation from the derived active and passive cloud property parameters. Remote Sensing of Environment, 248, 111972.</li> </ol> <p>If you have any questions, please contact Prof. Jie Cheng (Jie_Cheng@bnu.edu.cn).</p>

opencc-by-4.0Aug 2023View details →
zenodo32/100

The Effects of Differential Tropospheric Error on the Measurement of Wide-swath Interferometric Altimetry

<p>Related dataset and codes for the paper "The Effects of Differential Tropospheric Error on the Measurement of Wide-swath Interferometric Altimetry" submitted to IEEE TGRS.</p>

opencc-by-4.0Oct 2023View details →
zenodo28/100

ELITE surface longwave net radiation: global 1km Swath 5-min SLNR - Aqua (2010.04-06)

<p>The <strong>E</strong>ssential therma<strong>L</strong> <strong>I</strong>nfrared remo<strong>T</strong>e s<strong>E</strong>nsing (<strong>ELITE</strong>) product suite currently has four types of products, including land surface temperature (LST: clear-sky and all-sky), emissivity (NBE: narrowband emissivity; BBE: broadband emissivity; and spectral emissivity), the component of surface radiation and energy budget (SLUR: surface longwave upwelling radiation; SLDR: surface longwave downward radiation SLDR; SLNR: surface longwave net radiation), and the component of Earth&rsquo;s radiation budget (OLR; outgoing longwave radiation; RSR: reflected solar radiation). The spatial-temporal resolutions of the ELITE products are mainly determined by the employed satellite data sources. For more information about ELITE products, please refer to the website (<a href="https://elite.bnu.edu.cn">https://elite.bnu.edu.cn</a>).</p> <p>This dataset is the ELITE global 1km instantaneous SLNR&nbsp;product ranging&nbsp;from 2000&nbsp;to 2022 (continuously updated). This dataset was generated from the Moderate Resolution Imaging Spectrometer (MODIS, Terra and Aqua) data using the algorithm developed by&nbsp; Cheng et al. (2016), Cheng et al. (2017), and Yang and Cheng. (2020).&nbsp;</p> <p>This is the ELITE SLNR (Aqua)&nbsp;product in 2010.04-2010.06.&nbsp;Please&nbsp;<a href="https://zenodo.org/deposit/8255865"><strong><em>click here</em></strong></a>&nbsp;to download the ELITE SLNR (Aqua) product in 2010.01-2010.03&nbsp;and&nbsp;<a href="https://zenodo.org/deposit/8255887"><strong><em>click here</em></strong></a>&nbsp;to download the ELITE SLNR (Aqua) product in 2010.07-2010.09.</p> <p><strong>Dataset Characteristics:</strong></p> <ul> <li>Spatial Coverage: Global</li> <li>Temporal Coverage: 2010</li> <li>Spatial Resolution: 1 km</li> <li>Temporal Resolution: 5min/instantaneous</li> <li>Data Format: hdf</li> <li>Scale: 0.05</li> <li>Offset: -1000</li> </ul> <p><strong>Citation&nbsp;</strong>(Please cite these papers when using the data)<strong>:</strong></p> <ol> <li>Cheng, J., &amp; Liang, S. (2016). Global estimates for high-spatial-resolution clear-sky land surface upwelling longwave radiation from MODIS data.&nbsp;IEEE Transactions on Geoscience and Remote Sensing,&nbsp;<em>54</em>(7), 4115-4129.</li> <li>Cheng J, Liang S, Wang W, et al. An efficient hybrid method for estimating clear‐sky surface downward longwave radiation from MODIS data. Journal of Geophysical Research: Atmospheres, 2017, 122(5): 2616-2630.</li> <li>Yang, F., &amp; Cheng, J. (2020). A framework for estimating cloudy sky surface downward longwave radiation from the derived active and passive cloud property parameters. Remote Sensing of Environment, 248, 111972.</li> </ol> <p>If you have any questions, please contact Prof. Jie Cheng (Jie_Cheng@bnu.edu.cn).</p>

opencc-by-4.0Aug 2023View details →
nasa28/100

CERES Clouds and Radiative Swath Aqua FM3 MODIS Edition2C

CER_CRS_Aqua-FM3-MODIS_Edition2c is the Clouds and the Earth's Radiant Energy System (CERES) Clouds and Radiative Swath (CRS) Aqua-Flight Model 3 (FM3) Moderate-Resolution Imaging Spectroradiometer (MODIS) Edition2C data product, which was collected using the CERES-FM3 instrument on the Aqua platform. Data collection for this product is complete. Note that more recent (2006) CRS Ed2C fields for untuned SW (upper left for all-sky globe and lower right for clear-sky ocean) show a bit more bias than does an average of the earlier (2002-2005) Clouds and Radiative Swath (CRS) Ed2B. CRS Ed2C (Ed2B) biases are evaluated concerning SSF Ed2C (Ed2B) observations, and those Single Scanner Footprint (SSF) observations do not include recent "Rev1" adjustments to observations.The CRS product contains one hour of instantaneous Clouds and the Earth's Radiant Energy System (CERES) data for a single scanner instrument. The CRS has all of the CERES SSF product data. For each CERES footprint on the SSF, the CRS also contains vertical flux profiles evaluated at four levels in the atmosphere: the surface, 500-, 70-, and 1-hPa. The CRS fluxes and cloud parameters are adjusted for consistency with a radiative transfer model, and adjusted fluxes are evaluated at the four atmospheric levels for both clear-sky and total-sky.CERES is a key Earth Observing System (EOS) program component. The CERES instruments provide radiometric measurements of the Earth's atmosphere from three broadband channels. The CERES missions follow the successful Earth Radiation Budget Experiment (ERBE) mission. The first CERES instrument, the proto flight model (PFM), was launched on November 27, 1997, as part of the Tropical Rainfall Measuring Mission (TRMM). Two CERES instruments (FM1 and FM2) were launched into polar orbit on board the Earth Observing System (EOS) flagship Terra on December 18, 1999. Two additional CERES instruments (FM3 and FM4) were launched on board Earth Observing System (EOS) Aqua on May 4, 2002. The CERES FM5 instrument was launched on board the Suomi National Polar-orbiting Partnership (NPP) satellite on October 28, 2011. The newest CERES instrument (FM6) was launched on board the Joint Polar-Orbiting Satellite System 1 (JPSS-1) satellite, now called NOAA-20, on November 18, 2017.

restrictednotspecifiedApr 2025View details →
nasa28/100

GEOS-5 FP-IT Assimilation Geo-colocated to OMI/Aura UV-2 1-Orbit L2 Support Swath 13x24km V3 (OMUFPITMET) at GES DISC

The GEOS-5 FP-IT Assimilation Geo-colocated to OMI/Aura UV-2 1-Orbit L2 Support Swath 13x24km (OMUFPITMET) provides selected parameters from GEOS-5 Forward Processing for Instrument Teams (FP-IT) assimilated product produced by the Global Modeling and Assimilation Office (GMAO) co-located in space and time with the OMI UV-2 swath. The fields in this product include surface pressure, vertical temperature profiles, surface and vertical wind profiles, tropopause pressure, boundary layer top pressure, and surface geopotenial. The OMI team also provides a corresponding product for the OMI VIS swath, OMVFPITMET. The product has been generated for convenient use by the OMI/Aura team in their L2 algorithms, and for research where those L2 products are used. The original GEOS-5 FP-IT data are reported on a 0.625 deg longitude by 0.5 deg latitude grid, whereas the OMI UV-2 spatial resolution is 13km x 24km at nadir. To reduce the size of each orbital file, FP-IT data fields with a vertical dimension of 72 layers have been reduced to 47 layers in OMUFPITMET by combining layers above the troposphere. The OMUFPITMET files are in netCDF4 format which is compatible with most HDF5 readers and tools. Each file is approximately 45mb in size. The lead for this product is Zachary Fasnacht of SSAI. Joanna Joiner is the responsible NASA official.

restrictednotspecifiedApr 2025View details →

ScienceDex guides

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These curated guides explain access requirements, typical timelines, costs, and reuse considerations for widely used research datasets.

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Allen Brain Atlas

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Last verified 2026-04-30Open record

Annotated Behaviour and Observability Dataset (ABODe)

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DANDI Archive for NWB datasets

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dandi-nwb
electrophysiologyopenPublished Dandiset metadata and archive endpoints are available through the production DANDI API.
Last verified 2026-04-30Open record

International Brain Laboratory public data

The International Brain Laboratory public data releases expose standardized mouse decision-making experiments, including Neuropixels recordings, widefield calcium imaging, behavior, and session metadata accessed through the ONE API.

ibl
behavioral-neuroscienceopenPublic sessions can be searched and loaded from the IBL public data server through ONE.
Last verified 2026-04-29Open record

OpenNeuro

OpenNeuro is a free, open platform for sharing neuroimaging datasets, with public search, dataset pages, and download paths for web, S3, DataLad, and the OpenNeuro CLI.

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neuroscienceopenPublished datasets are available on demand over the internet.
Last verified 2026-04-29Open record