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Journal articles on the topic 'CALIPSO (satellite de télédétection)'

Author: Grafiati

Published: 25 May 2024

Last updated: 31 July 2025

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1

Chiriaco, M., H. Chepfer, P. Minnis, et al. "Comparison of CALIPSO-Like, LaRC, and MODIS Retrievals of Ice-Cloud Properties over SIRTA in France and Florida during CRYSTAL-FACE." Journal of Applied Meteorology and Climatology 46, no. 3 (2007): 249–72. http://dx.doi.org/10.1175/jam2435.1.

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Abstract This study compares cirrus-cloud properties and, in particular, particle effective radius retrieved by a Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observation (CALIPSO)-like method with two similar methods using Moderate-Resolution Imaging Spectroradiometer (MODIS), MODIS Airborne Simulator (MAS), and Geostationary Operational Environmental Satellite imagery. The CALIPSO-like method uses lidar measurements coupled with the split-window technique that uses the infrared spectral information contained at the 8.65-, 11.15-, and 12.05-μm bands to infer the microphysical propert

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Winker, D. M., J. Pelon, J. A. Coakley, et al. "The CALIPSO Mission." Bulletin of the American Meteorological Society 91, no. 9 (2010): 1211–30. http://dx.doi.org/10.1175/2010bams3009.1.

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Aerosols and clouds have important effects on Earth's climate through their effects on the radiation budget and the cycling of water between the atmosphere and Earth's surface. Limitations in our understanding of the global distribution and properties of aerosols and clouds are partly responsible for the current uncertainties in modeling the global climate system and predicting climate change. The CALIPSO satellite was developed as a joint project between NASA and the French space agency CNES to provide needed capabilities to observe aerosols and clouds from space. CALIPSO carries CALIOP, a tw

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Lacour, Adrien, Helene Chepfer, Matthew D. Shupe, et al. "Greenland Clouds Observed in CALIPSO-GOCCP: Comparison with Ground-Based Summit Observations." Journal of Climate 30, no. 15 (2017): 6065–83. http://dx.doi.org/10.1175/jcli-d-16-0552.1.

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Spaceborne lidar observations from the Cloud–Aerosol Lidar and Infrared Pathfinder Satellite Observations ( CALIPSO) satellite provide the first-ever observations of cloud vertical structure and phase over the entire Greenland Ice Sheet. This study leverages CALIPSO observations over Greenland to pursue two investigations. First, the GCM-Oriented CALIPSO Cloud Product ( CALIPSO-GOCCP) observations are compared with collocated ground-based radar and lidar observations at Summit, Greenland. The liquid cloud cover agrees well between the spaceborne and ground-based observations. In contrast, grou

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4

Ma, X., K. Bartlett, K. Harmon, and F. Yu. "Comparison of AOD between CALIPSO and MODIS: significant differences over major dust and biomass burning regions." Atmospheric Measurement Techniques Discussions 5, no. 6 (2012): 8343–67. http://dx.doi.org/10.5194/amtd-5-8343-2012.

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Abstract. Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observations (CALIPSO) provide, for the first time, global vertical profiles of aerosol optical properties, but further research is needed to evaluate the CALIPSO products. In this study, we employed about 6 yr (2006–2011) of CALIPSO level-3 monthly mean gridded aerosol optical depth (AOD) products (daytime and nighttime), for cloud free conditions, to compare with the MODIS Terra/Aqua level-3 monthly mean AOD dataset for the same time period. While the spatial distribution and seasonal variability of CALIPSO AOD is generally cons

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Ma, X., K. Bartlett, K. Harmon, and F. Yu. "Comparison of AOD between CALIPSO and MODIS: significant differences over major dust and biomass burning regions." Atmospheric Measurement Techniques 6, no. 9 (2013): 2391–401. http://dx.doi.org/10.5194/amt-6-2391-2013.

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Abstract. Cloud–Aerosol Lidar and Infrared Pathfinder Satellite Observations (CALIPSO) provide global vertical profiles of aerosol optical properties for the first time. In this study, we employed about 6 yr (2006–2011) of CALIPSO level 3 monthly mean gridded aerosol optical depth (AOD) products (daytime and nighttime) for cloud-free conditions, to compare with the Moderate Resolution Imaging Spectroradiometer (MODIS) Terra/Aqua level 3 monthly mean AOD dataset for the same time period. While the spatial distribution and seasonal variability of CALIPSO AOD is generally consistent with that of

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Zhao, Yinan, Qingxin Tang, Zhenting Hu, Quanzhou Yu, and Tianquan Liang. "Comparison and Analysis of CALIPSO Aerosol Optical Depth and AERONET Aerosol Optical Depth Products in Asia from 2006 to 2023." Remote Sensing 16, no. 23 (2024): 4359. http://dx.doi.org/10.3390/rs16234359.

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Aerosol optical depth (AOD) serves as a significant parameter in aerosol research. With the increasing utilization of satellite data in AOD research, it is crucial to evaluate the satellite AOD data. Using Aerosol Robotic Network (AERONET) in situ measurements, this study investigates the accuracy and applicability of Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observations (CALIPSO) AOD data in Asia from June 2006 to June 2023. By matching the CALIPSO AOD data in a 1° × 1° area around the selected AERONET sites, various statistical metrics were used to create a comprehensive evaluat

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7

Charbonneau, Lise, Denis Morin, and Richard Brochu. "Détection des unités d’utilisation et de couverture du sol urbain au moyen d’une simulation SPOT." Cahiers de géographie du Québec 29, no. 76 (2005): 29–47. http://dx.doi.org/10.7202/021692ar.

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La méthode utilisée consiste à classifier l'utilisation et la couverture du sol de l'agglomération urbaine de Sherbrooke avec l'aide d'images numériques acquises par un capteur aéroporté. Un survol de simulation du futur satellite SPOT a été effectué sur la région de Sherbrooke à l'aide du balayeur Daedalus multibande (DS1260) du Centre canadien de télédétection. Ce survol nous a permis d'estimer les possibilités du futur satellite SPOT pour la détection des phénomènes urbains. La télédétection des zones urbaines permettra la cartographie de ces unités d'utilisation et de couverture du sol ain

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8

Zou, Ling, Sabine Griessbach, Lars Hoffmann, Bing Gong, and Lunche Wang. "Revisiting global satellite observations of stratospheric cirrus clouds." Atmospheric Chemistry and Physics 20, no. 16 (2020): 9939–59. http://dx.doi.org/10.5194/acp-20-9939-2020.

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Abstract. As knowledge about the cirrus clouds in the lower stratosphere is limited, reliable long-term measurements are needed to assess their characteristics, radiative impact and important role in upper troposphere and lower stratosphere (UTLS) chemistry. We used 6 years (2006–2012) of Michelson Interferometer for Passive Atmospheric Sounding (MIPAS) measurements to investigate the global and seasonal distribution of stratospheric cirrus clouds and compared the MIPAS results with results derived from the latest version (V4.x) of the Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Obse

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Nagovitsyna, Ekaterina S., Sergey K. Dzholumbetov, Alexander A. Karasev, and Vassily A. Poddubny. "A Regional Aerosol Model for the Middle Urals Based on CALIPSO Measurements." Atmosphere 15, no. 1 (2023): 48. http://dx.doi.org/10.3390/atmos15010048.

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The present work aims to develop a regional Middle Urals Aerosol model (MUrA model) based on the joint analysis of long-term ground-based photometric measurements of the Aerosol Robotic NETwork (AERONET) and the results of lidar measurements of the CALIPSO (Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observation) satellite relying on information on the air trajectories at different altitudes calculated using the HYSPLIT (Hybrid Single Particle Lagrangian Integrated Trajectory model) software package. The MUrA model contains parameters of normalized volume size distributions (NVSDs) c

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Mona, L., G. Pappalardo, A. Amodeo, et al. "One year of CNR-IMAA multi-wavelength Raman lidar measurements in correspondence of CALIPSO overpass: Level 1 products comparison." Atmospheric Chemistry and Physics Discussions 9, no. 2 (2009): 8429–68. http://dx.doi.org/10.5194/acpd-9-8429-2009.

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Abstract. At CNR-IMAA, an aerosol lidar system is operative since May 2000 in the framework of EARLINET (European Aerosol Research Lidar Network), the first lidar network for tropospheric aerosol study on continental scale. High quality multi-wavelength measurements make this system a reference point for the validation of data products provided by CALIPSO (Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observations), the first satellite-borne lidar specifically designed for aerosol and cloud study. Since 14 June 2006, devoted measurements are performed at CNR-IMAA in coincidence of CALI

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Mona, L., G. Pappalardo, A. Amodeo, et al. "One year of CNR-IMAA multi-wavelength Raman lidar measurements in coincidence with CALIPSO overpasses: Level 1 products comparison." Atmospheric Chemistry and Physics 9, no. 18 (2009): 7213–28. http://dx.doi.org/10.5194/acp-9-7213-2009.

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Abstract. At CNR-IMAA, an aerosol lidar system has operated since May 2000 in the framework of EARLINET (European Aerosol Research Lidar Network), the first lidar network for tropospheric aerosol study on a continental scale. High quality multi-wavelength measurements make this system a reference point for the validation of data products provided by CALIPSO (Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observations), the first satellite-borne lidar specifically designed for aerosol and cloud study. Since 14 June 2006, dedicated measurements have been performed at CNR-IMAA in coinciden

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12

Hunt, William H., David M. Winker, Mark A. Vaughan, Kathleen A. Powell, Patricia L. Lucker, and Carl Weimer. "CALIPSO Lidar Description and Performance Assessment." Journal of Atmospheric and Oceanic Technology 26, no. 7 (2009): 1214–28. http://dx.doi.org/10.1175/2009jtecha1223.1.

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Abstract This paper provides background material for a collection of Cloud–Aerosol Lidar with Orthogonal Polarization (CALIOP) algorithm papers that are to be published in the Journal of Atmospheric and Oceanic Technology. It provides a brief description of the design and performance of CALIOP, a three-channel elastic backscatter lidar on the Cloud–Aerosol Lidar and Infrared Pathfinder Satellite Observation (CALIPSO) satellite. After more than 2 yr of on-orbit operation, CALIOP performance continues to be excellent in the key areas of laser energy, signal-to-noise ratio, polarization sensitivi

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Zhang, Ziyue, Miao Zhang, Muhammad Bilal, Bo Su, Chun Zhang, and Liuna Guo. "Comparison of MODIS- and CALIPSO-Derived Temporal Aerosol Optical Depth over Yellow River Basin (China) from 2007 to 2015." Earth Systems and Environment 4, no. 3 (2020): 535–50. http://dx.doi.org/10.1007/s41748-020-00181-7.

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Abstract In this study, Collection 6.1 (C6.1) of different aerosol optical depth (AOD) products of different spatial resolutions were used from the aqua moderate resolution imaging spectroradiometer (MODIS) including dark target (DT), deep blue (DB), deep blue (DB), and DT-DB (DTB). These products were compared with cloud-aerosol lidar, and infrared pathfinder satellite observation (CALIPSO) AOD retrievals over the Yellow River Basin (YERB), China from 2003 to 2017. The YERB was divided into three sub-regions, namely YERB1 (the mountainous terrain in the upper reaches of the YERB), YERB2 (the

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Mamouri, R. E., V. Amiridis, A. Papayannis, E. Giannakaki, G. Tsaknakis, and D. S. Balis. "Validation of CALIPSO space-borne-derived attenuated backscatter coefficient profiles using a ground-based lidar in Athens, Greece." Atmospheric Measurement Techniques 2, no. 2 (2009): 513–22. http://dx.doi.org/10.5194/amt-2-513-2009.

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Abstract. We present initial aerosol validation results of the space-borne lidar CALIOP -onboard the CALIPSO satellite- Level 1 attenuated backscatter coefficient profiles, using coincident observations performed with a ground-based lidar in Athens, Greece (37.9° N, 23.6° E). A multi-wavelength ground-based backscatter/Raman lidar system is operating since 2000 at the National Technical University of Athens (NTUA) in the framework of the European Aerosol Research LIdar NETwork (EARLINET), the first lidar network for tropospheric aerosol studies on a continental scale. Since July 2006, a total

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Georgoulias, Aristeidis K., Eleni Marinou, Alexandra Tsekeri, et al. "A First Case Study of CCN Concentrations from Spaceborne Lidar Observations." Remote Sensing 12, no. 10 (2020): 1557. http://dx.doi.org/10.3390/rs12101557.

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We present here the first cloud condensation nuclei (CCN) concentration profiles derived from measurements with the Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP) aboard the Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observations (CALIPSO), for different aerosol types at a supersaturation of 0.15%. CCN concentrations, along with the corresponding uncertainties, were inferred for a nighttime CALIPSO overpass on 9 September 2011, with coincident observations with the Facility for Airborne Atmospheric Measurements (FAAM) BAe-146 research aircraft, within the framework of the

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Folger, Kathrin, and Martin Weissmann. "Lidar-Based Height Correction for the Assimilation of Atmospheric Motion Vectors." Journal of Applied Meteorology and Climatology 55, no. 10 (2016): 2211–27. http://dx.doi.org/10.1175/jamc-d-15-0260.1.

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AbstractThis study uses lidar observations from the polar-orbiting Cloud–Aerosol Lidar and Infrared Pathfinder Satellite Observations (CALIPSO) satellite to correct operational atmospheric motion vector (AMV) pressure heights. This intends to reduce the height assignment error of AMVs for their use in data assimilation. Additionally, AMVs are treated as winds in a vertical layer as proposed by several recent studies. Corrected and uncorrected AMV winds are evaluated using short-term forecasts of the global forecasting system of the German Weather Service. First, a direct lidar-based height rea

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Choudhury, Goutam, and Matthias Tesche. "A first global height-resolved cloud condensation nuclei data set derived from spaceborne lidar measurements." Earth System Science Data 15, no. 8 (2023): 3747–60. http://dx.doi.org/10.5194/essd-15-3747-2023.

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Abstract. We present a global multiyear height-resolved data set of aerosol-type-specific cloud condensation nuclei concentrations (nCCN) estimated from the spaceborne lidar aboard the Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observation (CALIPSO) satellite. For estimating nCCN, we apply the recently introduced Optical Modelling of the CALIPSO Aerosol Microphysics (OMCAM) algorithm to the CALIPSO Level 2 Aerosol Profile product. The estimated nCCN are then gridded into a uniform latitude–longitude grid of 2∘×5∘, a vertical grid of resolution 60 m from the surface to an altitude of

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Lopes, F. J. S., E. Landulfo, and M. A. Vaughan. "Evaluating CALIPSO's 532 nm lidar ratio selection algorithm using AERONET sun photometers in Brazil." Atmospheric Measurement Techniques 6, no. 11 (2013): 3281–99. http://dx.doi.org/10.5194/amt-6-3281-2013.

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Abstract. Since the Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observations (CALIPSO) satellite first began probing the Earth's atmosphere on 13 June 2006, several research groups dedicated to investigating the atmosphere's optical properties have conducted measurement campaigns to validate the CALIPSO data products. Recently, in order to address the lack of CALIPSO validation studies in the Southern Hemisphere, and especially the South American continent, the Lasers Environmental Applications Research Group at Brazil's Nuclear and Energy Research Institute (IPEN) initiated efforts

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Rodier, S., Y. Hu, and M. Vaughan. "Sea ice detection with space-based LIDAR." Cryosphere Discussions 7, no. 5 (2013): 4681–701. http://dx.doi.org/10.5194/tcd-7-4681-2013.

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Abstract. Monitoring long-term climate change in the Polar Regions relies on accurate, detailed and repeatable measurements of geophysical processes and states. These regions are among the Earth's most vulnerable ecosystems, and measurements there have shown rapid changes in the seasonality and the extent of snow and sea ice coverage. The authors have recently developed a promising new technique that uses lidar surface measurements from the Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observations (CALIPSO) mission to infer ocean surface ice-water phase. CALIPSO's 532 nm depolarizatio

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Yang, B. Y., J. Liu, and X. Jia. "CORRECTION FOR THE CIRRUS CLOUD TOP HEIGHT OF MODIS BASED ON CALIPSO IN BEIJING-TIANJIN-HEBEI REGION." ISPRS - International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences XLII-3/W9 (October 25, 2019): 203–10. http://dx.doi.org/10.5194/isprs-archives-xlii-3-w9-203-2019.

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Abstract. Cirrus plays an important role in atmospheric radiation. It affects weather system and climate change. Satellite remote sensing is an important kind of observation for cloud. As a passive remote sensing instrument, large bias was found for thin cirrus cloud top height retrieval from MODIS (Moderate Resolution Imaging Spectroradiometer). Comparatively, CALIOP (Cloud-Aerosol Lidar with Orthogonal Polarization) aboard CALIPSO (Cloud–Aerosol Lidar and Infrared Pathfinder Satellite Observation) which is an active remote sensing instrument can acquire more accurate characteristics of thin

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Jankondee, Yuttapichai, Wilawan Kumharn, Choedtrakoo Homchampa, Oradee Pilahome, and Waichaya Nissawan. "PM2.5 modeling based on CALIPSO in bangkok." Creative Science 16, no. 3 (2024): 257117. http://dx.doi.org/10.55674/cs.v16i3.257117.

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Air quality has become a severe issue in Bangkok, mainly due to PM2.5 (fine particulate matter with particle size less than 2.5 μm). Aerosol optical depth (AOD) obtained for active satellite data has been widely used to estimate PM2.5 near the ground. Nevertheless, passive satellite data are rarely used to estimate PM2.5 near the ground. In this study, a total AOD in troposphere data achieved from the Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP) was used to determine PM2.5 with climate parameters (Temperature (TEM), relative humidity (RH), wind speed (WS), boundary layer height (B

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Padonou, Mikhaïl J. D. D., Antoine Denis, Yvon-Carmen H. Hountondji, Bernard Tychon, and Gérard N. Gouwakinnou. "Indicateurs de durabilité écologique des agroécosystèmes dérivés de la télédétection satellitaire : revue systématique." Cahiers Agricultures 33 (2024): 27. http://dx.doi.org/10.1051/cagri/2024022.

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Le suivi de la durabilité écologique des agroécosystèmes est nécessaire pour atténuer les impacts négatifs de l’agriculture sur l’environnement. Le développement de l’observation de la terre par satellite permet ce suivi sur de larges zones. Plusieurs indicateurs dérivés de la télédétection satellitaire permettent de le faire. Cette étude propose un inventaire des indicateurs de durabilité écologique (IDE) des agroécosystèmes dérivés de la télédétection satellitaire. Les bases de données Web of Science et Environmental Science Collection ont été explorées à partir d’une équation de recherche.

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Brunke, M. A., S. P. de Szoeke, P. Zuidema, and X. Zeng. "A comparison of ship and satellite measurements of cloud properties in the southeast Pacific stratus deck." Atmospheric Chemistry and Physics Discussions 10, no. 2 (2010): 3301–18. http://dx.doi.org/10.5194/acpd-10-3301-2010.

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Abstract. Here, liquid water path (LWP), cloud fraction, cloud top height, and cloud base height are retrieved by a suite of satellite instruments (the CPR aboard CloudSat, CALIOP aboard CALIPSO, and MODIS aboard Aqua) and compared to ship observations from research cruises made in 2001 and 2003–2007 into the stratus/stratocumulus deck over the southeast Pacific Ocean. It is found that CloudSat LWP is generally too high over this region and the CloudSat/CALIPSO cloud bases are too low which is to be expected from the increased sensitivity to precipitation by both the radar and lidar. This resu

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Balmes, Kelly, and Qiang Fu. "An Investigation of Optically Very Thin Ice Clouds from Ground-Based ARM Raman Lidars." Atmosphere 9, no. 11 (2018): 445. http://dx.doi.org/10.3390/atmos9110445.

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Optically very thin ice clouds from the Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observations (CALIPSO) and ground-based Raman lidars (RL) at the atmospheric radiation measurement (ARM) sites of the Southern Great Plains (SGP) and Tropical Western Pacific (TWP) are analyzed. The optically very thin ice clouds, with ice cloud column optical depths below 0.01, are about 23% of the transparent ice-cloudy profiles from the RL, compared to 4–7% from CALIPSO. The majority (66–76%) of optically very thin ice clouds from the RLs are found to be adjacent to ice clouds with ice cloud column

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Nam, Christine C. W., and Johannes Quaas. "Evaluation of Clouds and Precipitation in the ECHAM5 General Circulation Model Using CALIPSO and CloudSat Satellite Data." Journal of Climate 25, no. 14 (2012): 4975–92. http://dx.doi.org/10.1175/jcli-d-11-00347.1.

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Abstract Observations from Cloud–Aerosol Lidar and Infrared Pathfinder Satellite Observations (CALIPSO) and CloudSat satellites are used to evaluate clouds and precipitation in the ECHAM5 general circulation model. Active lidar and radar instruments on board CALIPSO and CloudSat allow the vertical distribution of clouds and their optical properties to be studied on a global scale. To evaluate the clouds modeled by ECHAM5 with CALIPSO and CloudSat, the lidar and radar satellite simulators of the Cloud Feedback Model Intercomparison Project’s Observation Simulator Package are used. Comparison of

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Lopes, F. J. S., E. Landulfo, and M. A. Vaughan. "Assessment of the CALIPSO Lidar 532 nm version 3 lidar ratio models using a ground-based lidar and AERONET sun photometers in Brazil." Atmospheric Measurement Techniques Discussions 6, no. 1 (2013): 1143–99. http://dx.doi.org/10.5194/amtd-6-1143-2013.

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Abstract. Since the Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observations (CALIPSO) satellite first began probing the Earth's atmosphere on 13 June 2006, several research groups dedicated to investigating the atmosphere's optical properties have conducted measurement campaigns to validate the CALIPSO data products. Recently, in order to address the lack of CALIPSO validation studies in the Southern Hemisphere, and especially the South American continent, the Lasers Environmental Applications Research Group at Brazil's Nuclear and Energy Research Institute (IPEN) initiated efforts

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Blanchard, Yann, Jacques Pelon, Edwin W. Eloranta, Kenneth P. Moran, Julien Delanoë, and Geneviève Sèze. "A Synergistic Analysis of Cloud Cover and Vertical Distribution from A-Train and Ground-Based Sensors over the High Arctic Station Eureka from 2006 to 2010." Journal of Applied Meteorology and Climatology 53, no. 11 (2014): 2553–70. http://dx.doi.org/10.1175/jamc-d-14-0021.1.

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AbstractActive remote sensing instruments such as lidar and radar allow one to accurately detect the presence of clouds and give information on their vertical structure and phase. To better address cloud radiative impact over the Arctic area, a combined analysis based on lidar and radar ground-based and A-Train satellite measurements was carried out to evaluate the efficiency of cloud detection, as well as cloud type and vertical distribution, over the Eureka station (80°N, 86°W) between June 2006 and May 2010. Cloud–Aerosol Lidar and Infrared Pathfinder Satellite Observations (CALIPSO) and Cl

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Papagiannopoulos, N., L. Mona, L. Alados-Arboledas, et al. "CALIPSO climatological products: evaluation and suggestions from EARLINET." Atmospheric Chemistry and Physics Discussions 15, no. 21 (2015): 31197–246. http://dx.doi.org/10.5194/acpd-15-31197-2015.

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Abstract. The CALIPSO Level 3 (CL3) product, available since December 2011, is the most recent data set produced by the observations of the Cloud–Aerosol Lidar with Orthogonal Polarization (CALIOP) instrument onboard the Cloud–Aerosol Lidar and Pathfinder Satellite Observations (CALIPSO) space platform. The European Aerosol Research Lidar Network (EARLINET), based mainly on multi-wavelength Raman lidar systems, is the most appropriate ground-based reference for CALIPSO calibration/validation studies on a continental scale. In this work, CALIPSO data are compared against EARLINET monthly averag

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Papagiannopoulos, Nikolaos, Lucia Mona, Lucas Alados-Arboledas, et al. "CALIPSO climatological products: evaluation and suggestions from EARLINET." Atmospheric Chemistry and Physics 16, no. 4 (2016): 2341–57. http://dx.doi.org/10.5194/acp-16-2341-2016.

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Abstract. The CALIPSO Level 3 (CL3) product is the most recent data set produced by the observations of the Cloud–Aerosol Lidar with Orthogonal Polarization (CALIOP) instrument onboard the Cloud–Aerosol Lidar and Pathfinder Satellite Observations (CALIPSO) space platform. The European Aerosol Research Lidar Network (EARLINET), based mainly on multi-wavelength Raman lidar systems, is the most appropriate ground-based reference for CALIPSO calibration/validation studies on a continental scale. In this work, CALIPSO data are compared against EARLINET monthly averaged profiles obtained by measurem

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Khalesifard, Hamid R., and Farizeh Bayat. "Calipso recordings and monitoring dust storms over the open seas in south of the iran plateau." EPJ Web of Conferences 176 (2018): 05027. http://dx.doi.org/10.1051/epjconf/201817605027.

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Open seas in the south of the Iran plateau are under the influence of heavy dust storms which are originating either from the Tigris and Euphrates basin, the Arabian Peninsula or Hamoun lake. We have used the recordings of the CALIPSO satellite to investigate the seasonal variations as well as the origins of the dust storms over the region. CALIPSO data set shows dust activities are frequent during May to September in the interested region and the Hamoun lake has considerable impacts on it.

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Jin, Hongchun, and Shaima L. Nasiri. "Evaluation of AIRS Cloud-Thermodynamic-Phase Determination with CALIPSO." Journal of Applied Meteorology and Climatology 53, no. 4 (2014): 1012–27. http://dx.doi.org/10.1175/jamc-d-13-0137.1.

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AbstractAtmospheric Infrared Sounder (AIRS) infrared-based cloud-thermodynamic-phase retrievals are evaluated using the Cloud–Aerosol Lidar and Infrared Pathfinder Satellite Observations (CALIPSO) cloud thermodynamic phase. The AIRS cloud phase is derived from spectral information contained within the 8–12-μm window, and CALIPSO provides coincident pixel-scale observations of cloud phase using the depolarization capability of the 532-nm channel. Comparisons are performed between the AIRS and CALIPSO cloud-phase observations for single-layer (48.5% of all clouds), heterogeneous-layer (45.9%), a

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Delanoë, Julien, Alain Protat, Olivier Jourdan, et al. "Comparison of Airborne In Situ, Airborne Radar–Lidar, and Spaceborne Radar–Lidar Retrievals of Polar Ice Cloud Properties Sampled during the POLARCAT Campaign." Journal of Atmospheric and Oceanic Technology 30, no. 1 (2013): 57–73. http://dx.doi.org/10.1175/jtech-d-11-00200.1.

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Abstract This study illustrates the high potential of RALI, the French airborne radar–lidar instrument, for studying cloud processes and evaluating satellite products when satellite overpasses are available. For an Arctic nimbostratus ice cloud collected on 1 April 2008 during the Polar Study using Aircraft, Remote Sensing, Surface Measurements and Models, of Climate, Chemistry, Aerosols, and Transport (POLARCAT) campaign, the capability of this synergistic instrument to retrieve cloud properties and to characterize the cloud phase at scales smaller than a kilometer, which is crucial for cloud

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Liu, Boming, Yingying Ma, Jiqiao Liu, Wei Gong, Wei Wang, and Ming Zhang. "Graphics algorithm for deriving atmospheric boundary layer heights from CALIPSO data." Atmospheric Measurement Techniques 11, no. 9 (2018): 5075–85. http://dx.doi.org/10.5194/amt-11-5075-2018.

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Abstract. The atmospheric boundary layer is an important atmospheric feature that affects environmental health and weather forecasting. In this study, we proposed a graphics algorithm for the derivation of atmospheric boundary layer height (BLH) from the Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observations (CALIPSO) data. Owing to the differences in scattering intensity between molecular and aerosol particles, the total attenuated backscatter coefficient 532 and attenuated backscatter coefficient 1064 were used simultaneously for BLH detection. The proposed algorithm transformed

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Richardson, Mark, Jussi Leinonen, Heather Q. Cronk, James McDuffie, Matthew D. Lebsock, and Graeme L. Stephens. "Marine liquid cloud geometric thickness retrieved from OCO-2's oxygen A-band spectrometer." Atmospheric Measurement Techniques 12, no. 3 (2019): 1717–37. http://dx.doi.org/10.5194/amt-12-1717-2019.

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Abstract. This paper introduces the OCO2CLD-LIDAR-AUX product, which uses the Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observation (CALIPSO) lidar and the Orbiting Carbon Observatory-2 (OCO-2) hyperspectral A-band spectrometer. CALIPSO provides a prior cloud top pressure (Ptop) for an OCO-2-based retrieval of cloud optical depth, Ptop and cloud geometric thickness expressed in hPa. Measurements are of single-layer liquid clouds over oceans from September 2014 to December 2016 when collocated data are available. Retrieval performance is best for solar zenith angles <45∘ and when

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Hu, Y., K. Stamnes, M. Vaughan, et al. "Sea surface wind speed estimation from space-based lidar measurements." Atmospheric Chemistry and Physics Discussions 8, no. 1 (2008): 2771–93. http://dx.doi.org/10.5194/acpd-8-2771-2008.

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Abstract. Global satellite observations of lidar backscatter measurements acquired by the Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observation (CALIPSO) mission and collocated sea surface wind speed data from the Advanced Microwave Scanning Radiometer for the Earth Observing System (AMSR-E), are used to investigate the relation between wind driven wave slope variance and sea surface wind speed. The new slope variance – wind speed relation established from this study is similar to the linear relation from Cox-Munk (1954) and the log-linear relation from Wu (1972, 1990) for wind spe

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Choudhury, Goutam, and Matthias Tesche. "Estimating cloud condensation nuclei concentrations from CALIPSO lidar measurements." Atmospheric Measurement Techniques 15, no. 3 (2022): 639–54. http://dx.doi.org/10.5194/amt-15-639-2022.

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Abstract. We present a novel methodology to estimate cloud condensation nuclei (CCN) concentrations from spaceborne CALIPSO (Cloud–Aerosol Lidar and Infrared Pathfinder Satellite Observations) lidar measurements. The algorithm utilizes (i) the CALIPSO-derived backscatter and extinction coefficient, depolarization ratio, and aerosol subtype information; (ii) the normalized volume size distributions and refractive indices from the CALIPSO aerosol model; and (iii) the MOPSMAP (modelled optical properties of ensembles of aerosol particles) optical modelling package. For each CALIPSO height bin, we

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Mamouri, R. E., V. Amiridis, A. Papayannis, E. Giannakaki, G. Tsaknakis, and D. S. Balis. "Validation of CALIPSO space-borne-derived aerosol vertical structures using a ground-based lidar in Athens, Greece." Atmospheric Measurement Techniques Discussions 2, no. 1 (2009): 561–87. http://dx.doi.org/10.5194/amtd-2-561-2009.

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Abstract. We present initial aerosol validation results of the space-borne lidar CALIOP retrievals -onboard the CALIPSO satellite-, using coincident observations performed with a ground-based lidar in Athens, Greece (37.9° N, 23.6° E). A multi-wavelength ground-based backscatter/Raman lidar system is operating since 2000 at the National Technical University of Athens (NTUA) in the framework of the European Aerosol Research LIdar NETwork (EARLINET), the first lidar network for tropospheric aerosol studies on a continental scale. Since July 2006, a total of 40 coincidental aerosol ground-based l

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Matsaguim Nguimdo, Cédric Aurélien, and Emmanuel D. Tiomo. "FORET D'ARBRES ALEATOIRES ET CLASSIFICATION D'IMAGES SATELLITES : RELATION ENTRE LA PRECISION DU MODELE D'ENTRAINEMENT ET LA PRECISION GLOBALE DE LA CLASSIFICATION." Revue Française de Photogrammétrie et de Télédétection, no. 222 (November 26, 2020): 3–14. http://dx.doi.org/10.52638/rfpt.2020.477.

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Résumé: En télédétection, il existe un grand nombre d'algorithmes permettant de classifier une image satellite. Parmi ces algorithmes de classification, la Forêt d'Arbres Aléatoires apparait comme particulièrement performant. Cette étude a pour objectifs d'évaluer (1) l'importance de la sélection des images pour le niveau de précision du modèle d'entrainement et (2) la nature de la relation qui existe entre le niveau de précision du modèle et celui de la précision globale de la carte thématique résultant de la classification de l'image satellite avec cet algorithme de classification. A partir

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Pitts, M. C., L. R. Poole, and L. W. Thomason. "CALIPSO polar stratospheric cloud observations: second-generation detection algorithm and composition discrimination." Atmospheric Chemistry and Physics Discussions 9, no. 2 (2009): 8121–57. http://dx.doi.org/10.5194/acpd-9-8121-2009.

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Abstract. This paper focuses on polar stratospheric cloud (PSC) measurements by the CALIOP (Cloud-Aerosol LIdar with Orthogonal Polarization) lidar system onboard the CALIPSO (Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observations) spacecraft, which has been operating since June 2006. We describe a second-generation PSC detection algorithm that utilizes both the CALIOP 532-nm scattering ratio (ratio of total-to-molecular backscatter coefficients) and 532-nm perpendicular backscatter coefficient measurements for cloud detection. The inclusion of the perpendicular backscatter measure

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Liu, Yinghui, Steven A. Ackerman, Brent C. Maddux, Jeffrey R. Key, and Richard A. Frey. "Errors in Cloud Detection over the Arctic Using a Satellite Imager and Implications for Observing Feedback Mechanisms." Journal of Climate 23, no. 7 (2010): 1894–907. http://dx.doi.org/10.1175/2009jcli3386.1.

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Abstract Arctic sea ice extent has decreased dramatically over the last 30 years, and this trend is expected to continue through the twenty-first century. Changes in sea ice extent impact cloud cover, which in turn influences the surface energy budget. Understanding cloud feedback mechanisms requires an accurate determination of cloud cover over the polar regions, which must be obtained from satellite-based measurements. The accuracy of cloud detection using observations from space varies with surface type, complicating any assessment of climate trends as well as the understanding of ice–albed

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Pitts, M. C., L. W. Thomason, L. R. Poole, and D. M. Winker. "Characterization of Polar Stratospheric Clouds with Space-Borne Lidar: CALIPSO and the 2006 Antarctic Season." Atmospheric Chemistry and Physics Discussions 7, no. 3 (2007): 7933–85. http://dx.doi.org/10.5194/acpd-7-7933-2007.

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Abstract. The role of polar stratospheric clouds in polar ozone loss has been well documented. The CALIPSO satellite mission offers a new opportunity to characterize PSCs on spatial and temporal scales previously impossible. A PSC detection algorithm based on a single wavelength threshold approach has been developed for CALIPSO. The method appears to accurately detect PSCs of all opacities, including tenuous clouds, with a very low rate of false positives and few missed clouds. We applied the algorithm to CALIOP data acquired during the 2006 Antarctic winter season from 13 June through 31 Octo

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Pitts, M. C., L. W. Thomason, L. R. Poole, and D. M. Winker. "Characterization of Polar Stratospheric Clouds with spaceborne lidar: CALIPSO and the 2006 Antarctic season." Atmospheric Chemistry and Physics 7, no. 19 (2007): 5207–28. http://dx.doi.org/10.5194/acp-7-5207-2007.

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Abstract. The role of polar stratospheric clouds in polar ozone loss has been well documented. The CALIPSO satellite mission offers a new opportunity to characterize PSCs on spatial and temporal scales previously impossible. A PSC detection algorithm based on a single wavelength threshold approach has been developed for CALIPSO. The method appears to accurately detect PSCs of all opacities, including tenuous clouds, with a very low rate of false positives and few missed clouds. We applied the algorithm to CALIOP data acquired during the 2006 Antarctic winter season from 13 June through 31 Octo

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Karageorgopoulou, Archontoula, Elina Giannakaki, Christos Stathopoulos, et al. "CALIPSO Overpasses During Three Atmospheric Pollen Events Detected by Hirst-Type Volumetric Samplers in Two Urban Cities in Greece." Atmosphere 16, no. 3 (2025): 317. https://doi.org/10.3390/atmos16030317.

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Vertically retrieved optical properties by Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observations (CALIPSO) were investigated in the case of three selected events over Athens and Thessaloniki with documented high pollen concentrations. Hirst-type volumetric samplers were used to detect and characterize the pollen during the CALIPSO overpasses. Only cases with a total pollen concentration greater than 400 grains m−3 for at least two hours per day were considered severe pollen events, while model simulations were used to exclude the presence of other depolarizing aerosol types. This

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Carn, S. A., N. A. Krotkov, K. Yang, et al. "Extended observations of volcanic SO<sub>2</sub> and sulfate aerosol in the stratosphere." Atmospheric Chemistry and Physics Discussions 7, no. 1 (2007): 2857–71. http://dx.doi.org/10.5194/acpd-7-2857-2007.

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Abstract. Sulfate aerosol produced after injection of sulfur dioxide (SO2) into the stratosphere by volcanic eruptions can trigger climate change. We present new satellite data from the Ozone Monitoring Instrument (OMI) and Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observations (CALIPSO) missions that reveal the composition, structure and longevity of a stratospheric SO2 cloud and derived sulfate layer following a modest eruption (0.2 Tg total SO2) of Soufriere Hills volcano, Montserrat on 20 May 2006. The SO2 cloud alone was tracked for over 3 weeks and a distance of over 20 000 k

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Biondi, R., W. J. Randel, S. P. Ho, T. Neubert, and S. Syndergaard. "Thermal structure of intense convective clouds derived from GPS radio occultations." Atmospheric Chemistry and Physics Discussions 11, no. 10 (2011): 29093–116. http://dx.doi.org/10.5194/acpd-11-29093-2011.

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Abstract. Thermal structure associated with deep convective clouds is investigated using Global Positioning System (GPS) radio occultation measurements. GPS data are insensitive to the presence of clouds, and provide high vertical resolution and high accuracy measurements to identify associated temperature behavior. Deep convective systems are identified using International Satellite Cloud Climatology Project (ISCCP) satellite data, and cloud tops are accurately measured using Cloud-Aerosol Lidar with Orthogonal Polarization (CALIPSO) lidar observations; we focus on 53 cases of near-coincident

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Biondi, R., W. J. Randel, S. P. Ho, T. Neubert, and S. Syndergaard. "Thermal structure of intense convective clouds derived from GPS radio occultations." Atmospheric Chemistry and Physics 12, no. 12 (2012): 5309–18. http://dx.doi.org/10.5194/acp-12-5309-2012.

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Abstract. Thermal structure associated with deep convective clouds is investigated using Global Positioning System (GPS) radio occultation measurements. GPS data are insensitive to the presence of clouds, and provide high vertical resolution and high accuracy measurements to identify associated temperature behavior. Deep convective systems are identified using International Satellite Cloud Climatology Project (ISCCP) satellite data, and cloud tops are accurately measured using Cloud-Aerosol Lidar with Orthogonal Polarization (CALIPSO) lidar observations; we focus on 53 cases of near-coincident

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Viollier, Michel, Jacques Dupont, and J. Y. Balois. "Télédétection par satellite du matériel particulaire en suspension en Manche orientale." Hommes et Terres du Nord 3, no. 1 (1985): 230–33. http://dx.doi.org/10.3406/htn.1985.2004.

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Gong, Xin, Delong Xiu, Xiaoling Sun, et al. "Dust Aerosol Classification in Northwest China Using CALIPSO Data and an Enhanced 1D U-Net Network." Atmosphere 16, no. 7 (2025): 812. https://doi.org/10.3390/atmos16070812.

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Dust aerosols significantly affect climate and air quality in Northwest China (30–50° N, 70–110° E), where frequent dust storms complicate accurate aerosol classification when using CALIPSO satellite data. This study introduces an Enhanced 1D U-Net model to enhance dust aerosol retrieval, incorporating Inception modules for multi-scale feature extraction, Transformer blocks for global contextual modeling, CBAM attention mechanisms for improved feature selection, and residual connections for training stability. Using CALIPSO Level 1B and Level 2 Vertical Feature Mask (VFM) data from 2015 to 202

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Liu, Yinghui. "Impacts of active satellite sensors' low-level cloud detection limitations on cloud radiative forcing in the Arctic." Atmospheric Chemistry and Physics 22, no. 12 (2022): 8151–73. http://dx.doi.org/10.5194/acp-22-8151-2022.

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Abstract. Previous studies revealed that satellites sensors with the best detection capability identify 25 %–40 % and 0 %–25 % fewer clouds below 0.5 and between 0.5–1.0 km, respectively, over the Arctic. Quantifying the impacts of cloud detection limitations on the radiation flux are critical especially over the Arctic Ocean considering the dramatic changes in Arctic sea ice. In this study, the proxies of the space-based radar, CloudSat, and lidar, CALIPSO (Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observations), cloud masks are derived based on simulated radar reflectivity with Q

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Hu, Yongxiang, David Winker, Mark Vaughan, et al. "CALIPSO/CALIOP Cloud Phase Discrimination Algorithm." Journal of Atmospheric and Oceanic Technology 26, no. 11 (2009): 2293–309. http://dx.doi.org/10.1175/2009jtecha1280.1.

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Abstract The current cloud thermodynamic phase discrimination by Cloud-Aerosol Lidar Pathfinder Satellite Observations (CALIPSO) is based on the depolarization of backscattered light measured by its lidar [Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP)]. It assumes that backscattered light from ice crystals is depolarizing, whereas water clouds, being spherical, result in minimal depolarization. However, because of the relationship between the CALIOP field of view (FOV) and the large distance between the satellite and clouds and because of the frequent presence of oriented ice cryst

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