Articles | Volume 15, issue 7
https://doi.org/10.5194/essd-15-3223-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/essd-15-3223-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
A new sea ice concentration product in the polar regions derived from the FengYun-3 MWRI sensors
Ying Chen
Chinese Antarctic Center of Surveying and Mapping, Wuhan University, Wuhan, 430079, China
Ruibo Lei
Key Laboratory for Polar Science of the Ministry of Natural Resources, Polar Research Institute of China, Shanghai, China
Chinese Antarctic Center of Surveying and Mapping, Wuhan University, Wuhan, 430079, China
Xi Zhao
School of Geospatial Engineering and Science, Sun Yat-Sen University & Southern Marine Science and Engineering Guangdong Laboratory, Zhuhai, China
Shengli Wu
Key Laboratory of Radiometric Calibration and Validation for
Environmental Satellites, National Satellite Meteorological Center (National
Center for Space Weather), China Meteorological Administration, Beijing,
China
Innovation Center for FengYun Meteorological Satellite (FYSIC),
Beijing, China
Yue Liu
Jiangsu Provincial Surveying and Mapping Engineering Institute,
Nanjing, China
Chinese Antarctic Center of Surveying and Mapping, Wuhan University, Wuhan, 430079, China
Pei Fan
Chinese Antarctic Center of Surveying and Mapping, Wuhan University, Wuhan, 430079, China
Qing Ji
Chinese Antarctic Center of Surveying and Mapping, Wuhan University, Wuhan, 430079, China
Peng Zhang
Key Laboratory of Radiometric Calibration and Validation for
Environmental Satellites, National Satellite Meteorological Center (National
Center for Space Weather), China Meteorological Administration, Beijing,
China
Innovation Center for FengYun Meteorological Satellite (FYSIC),
Beijing, China
Xiaoping Pang
CORRESPONDING AUTHOR
Chinese Antarctic Center of Surveying and Mapping, Wuhan University, Wuhan, 430079, China
Related authors
Y. Chen, X. Zhao, M. Qu, Z. Cheng, X. Pang, and Q. Ji
Int. Arch. Photogramm. Remote Sens. Spatial Inf. Sci., XLIII-B3-2020, 861–867, https://doi.org/10.5194/isprs-archives-XLIII-B3-2020-861-2020, https://doi.org/10.5194/isprs-archives-XLIII-B3-2020-861-2020, 2020
Fanyi Zhang, Ruibo Lei, Meng Qu, Na Li, Ying Chen, and Xiaoping Pang
EGUsphere, https://doi.org/10.5194/egusphere-2024-2723, https://doi.org/10.5194/egusphere-2024-2723, 2024
Short summary
Short summary
We reconstructed sea ice drift trajectories and identified optimal deployment areas for Lagrangian observations. It revealed a preference for ice advection towards the Transpolar Drift region over the Beaufort Gyre, with endpoints influenced by large-scale atmospheric circulation patterns. This study could help the future ice camp/buoy deployment strategies, ensuring the sustainability of crucial Arctic observations in the face of changing environmental conditions.
Xinran Xia, Rubin Jiang, Min Min, Shengli Wu, Peng Zhang, and Xiangao Xia
Earth Syst. Sci. Data Discuss., https://doi.org/10.5194/essd-2024-395, https://doi.org/10.5194/essd-2024-395, 2024
Revised manuscript under review for ESSD
Short summary
Short summary
Based on the MicroWave Radiation Imager aboard FY-3 series satellites, we developed a global terrestrial precipitable water vapor dataset from 2012 to 2020. This dataset overcomes the limitations of infrared observations and provides accurate, all-weather PWV data ,spanning all types of land surface. Researchers are expected to leverage it to explore the role of water vapor in weather patterns, refine precipitation forecasting, and validate climate simulations.
Yi Zhou, Xianwei Wang, Ruibo Lei, Arttu Jutila, Donald K. Perovich, Luisa von Albedyll, Dmitry V. Divine, Yu Zhang, and Christian Haas
EGUsphere, https://doi.org/10.5194/egusphere-2024-2821, https://doi.org/10.5194/egusphere-2024-2821, 2024
Short summary
Short summary
This study examines how the bulk density of Arctic sea ice varies seasonally, a factor often overlooked in satellite measurements of sea ice thickness. From October to April, we found significant seasonal variations in sea ice bulk density at different spatial scales using direct observations as well as airborne and satellite data. New models were then developed to indirectly predict sea ice bulk density. This advance can improve our ability to monitor changes in Arctic sea ice.
Fangbo Pan, Lingmei Jiang, Gongxue Wang, Jinmei Pan, Jinyu Huang, Cheng Zhang, Huizhen Cui, Jianwei Yang, Zhaojun Zheng, Shengli Wu, and Jiancheng Shi
Earth Syst. Sci. Data, 16, 2501–2523, https://doi.org/10.5194/essd-16-2501-2024, https://doi.org/10.5194/essd-16-2501-2024, 2024
Short summary
Short summary
It is important to strengthen the continuous monitoring of snow cover as a key indicator of imbalance in the Asian Water Tower (AWT) region. We generate long-term daily gap-free fractional snow cover products over the AWT at 0.005° resolution from 2000 to 2022 based on the multiple-endmember spectral mixture analysis algorithm and the gap-filling algorithm. They can provide highly accurate, quantitative fractional snow cover information for subsequent studies on hydrology and climate.
Yi Zhou, Xianwei Wang, Ruibo Lei, Luisa von Albedyll, Donald K. Perovich, Yu Zhang, and Christian Haas
EGUsphere, https://doi.org/10.5194/egusphere-2024-1240, https://doi.org/10.5194/egusphere-2024-1240, 2024
Preprint archived
Short summary
Short summary
This study examines how the density of Arctic sea ice varies seasonally, a factor often overlooked in satellite measurements of sea ice thickness. From October to April, using direct observations and satellite data, we found that sea ice density decreases significantly until mid-January due to increased porosity as the ice ages, and then stabilizes until April. We then developed new models to estimate sea ice density. This advance can improve our ability to monitor changes in Arctic sea ice.
Yan Sun, Shaoyin Wang, Xiao Cheng, Teng Li, Chong Liu, Yufang Ye, and Xi Zhao
EGUsphere, https://doi.org/10.5194/egusphere-2024-1177, https://doi.org/10.5194/egusphere-2024-1177, 2024
Preprint archived
Short summary
Short summary
Arctic sea ice has rapidly declined due to global warming, leading to extreme weather events. Accurate ice monitoring is vital for understanding and forecasting these impacts. Combining SAR and AMSR2 data with machine learning is efficient but requires sufficient labels. We propose a framework integrating the U-Net model with the Multi-textRG algorithm to achieve ice-water classification at SAR-level resolution and to generate accurate labels for improved U-Net model training.
Zhenhao Wu, Yunfei Fu, Peng Zhang, Songyan Gu, and Lin Chen
Earth Syst. Sci. Data Discuss., https://doi.org/10.5194/essd-2023-532, https://doi.org/10.5194/essd-2023-532, 2024
Revised manuscript under review for ESSD
Short summary
Short summary
We establish a new rain cell precipitation parameter and visible infrared and microwave signal dataset combining with the multi-instrument observation data on the Tropical Rainfall Measuring Mission (TRMM). The purpose of this dataset is to promote the three-dimensional study of rain cell precipitation system, and reveal the spatial and temporal variations of the scale morphology and intensity of the system.
Miao Yu, Peng Lu, Matti Leppäranta, Bin Cheng, Ruibo Lei, Bingrui Li, Qingkai Wang, and Zhijun Li
The Cryosphere, 18, 273–288, https://doi.org/10.5194/tc-18-273-2024, https://doi.org/10.5194/tc-18-273-2024, 2024
Short summary
Short summary
Variations in Arctic sea ice are related not only to its macroscale properties but also to its microstructure. Arctic ice cores in the summers of 2008 to 2016 were used to analyze variations in the ice inherent optical properties related to changes in the ice microstructure. The results reveal changing ice microstructure greatly increased the amount of solar radiation transmitted to the upper ocean even when a constant ice thickness was assumed, especially in marginal ice zones.
Fanyi Zhang, Ruibo Lei, Mengxi Zhai, Xiaoping Pang, and Na Li
The Cryosphere, 17, 4609–4628, https://doi.org/10.5194/tc-17-4609-2023, https://doi.org/10.5194/tc-17-4609-2023, 2023
Short summary
Short summary
Atmospheric circulation anomalies lead to high Arctic sea ice outflow in winter 2020, causing heavy ice conditions in the Barents–Greenland seas, subsequently impeding the sea surface temperature warming. This suggests that the winter–spring Arctic sea ice outflow can be considered a predictor of changes in sea ice and other marine environmental conditions in the Barents–Greenland seas, which could help to improve our understanding of the physical connections between them.
Na Li, Ruibo Lei, Petra Heil, Bin Cheng, Minghu Ding, Zhongxiang Tian, and Bingrui Li
The Cryosphere, 17, 917–937, https://doi.org/10.5194/tc-17-917-2023, https://doi.org/10.5194/tc-17-917-2023, 2023
Short summary
Short summary
The observed annual maximum landfast ice (LFI) thickness off Zhongshan (Davis) was 1.59±0.17 m (1.64±0.08 m). Larger interannual and local spatial variabilities for the seasonality of LFI were identified at Zhongshan, with the dominant influencing factors of air temperature anomaly, snow atop, local topography and wind regime, and oceanic heat flux. The variability of LFI properties across the study domain prevailed at interannual timescales, over any trend during the recent decades.
Ruibo Lei, Mario Hoppmann, Bin Cheng, Marcel Nicolaus, Fanyi Zhang, Benjamin Rabe, Long Lin, Julia Regnery, and Donald K. Perovich
The Cryosphere Discuss., https://doi.org/10.5194/tc-2023-25, https://doi.org/10.5194/tc-2023-25, 2023
Manuscript not accepted for further review
Short summary
Short summary
To characterize the freezing and melting of different types of sea ice, we deployed four IMBs during the MOSAiC second drift. The drifting pattern, together with a large snow accumulation, relatively warm air temperatures, and a rapid increase in oceanic heat close to Fram Strait, determined the seasonal evolution of the ice mass balance. The refreezing of ponded ice and voids within the unconsolidated ridges amplifies the anisotropy of the heat exchange between the ice and the atmosphere/ocean.
Long Lin, Ruibo Lei, Mario Hoppmann, Donald K. Perovich, and Hailun He
The Cryosphere, 16, 4779–4796, https://doi.org/10.5194/tc-16-4779-2022, https://doi.org/10.5194/tc-16-4779-2022, 2022
Short summary
Short summary
Ice mass balance observations indicated that average basal melt onset was comparable in the central Arctic Ocean and approximately 17 d earlier than surface melt in the Beaufort Gyre. The average onset of basal growth lagged behind the surface of the pan-Arctic Ocean for almost 3 months. In the Beaufort Gyre, both drifting-buoy observations and fixed-point observations exhibit a trend towards earlier basal melt onset, which can be ascribed to the earlier warming of the surface ocean.
Yu Liang, Haibo Bi, Haijun Huang, Ruibo Lei, Xi Liang, Bin Cheng, and Yunhe Wang
The Cryosphere, 16, 1107–1123, https://doi.org/10.5194/tc-16-1107-2022, https://doi.org/10.5194/tc-16-1107-2022, 2022
Short summary
Short summary
A record minimum July sea ice extent, since 1979, was observed in 2020. Our results reveal that an anomalously high advection of energy and water vapor prevailed during spring (April to June) 2020 over regions with noticeable sea ice retreat. The large-scale atmospheric circulation and cyclones act in concert to trigger the exceptionally warm and moist flow. The convergence of the transport changed the atmospheric characteristics and the surface energy budget, thus causing a severe sea ice melt.
Yungang Wang, Liping Fu, Fang Jiang, Xiuqing Hu, Chengbao Liu, Xiaoxin Zhang, Jiawei Li, Zhipeng Ren, Fei He, Lingfeng Sun, Ling Sun, Zhongdong Yang, Peng Zhang, Jingsong Wang, and Tian Mao
Atmos. Meas. Tech., 15, 1577–1586, https://doi.org/10.5194/amt-15-1577-2022, https://doi.org/10.5194/amt-15-1577-2022, 2022
Short summary
Short summary
Far-ultraviolet (FUV) airglow radiation is particularly well suited for space-based remote sensing. The Ionospheric Photometer (IPM) instrument carried aboard the Feng Yun 3-D satellite measures the spectral radiance of the Earth FUV airglow. IPM is a tiny, highly sensitive, and robust remote sensing instrument. Initial results demonstrate that the performance of IPM meets the designed requirement and therefore can be used to study the thermosphere and ionosphere in the future.
Lin Tian, Lin Chen, Peng Zhang, and Lei Bi
Atmos. Chem. Phys., 21, 11669–11687, https://doi.org/10.5194/acp-21-11669-2021, https://doi.org/10.5194/acp-21-11669-2021, 2021
Short summary
Short summary
The result shows dust aerosols from the Taklimakan Desert have higher aerosol scattering during dust storm cases of this paper, and this caused higher negative direct radiative forcing efficiency (DRFEdust) than aerosols from the Sahara.
The microphysical properties and particle shapes of dust aerosol significantly influence DRFEdust. The satellite-based equi-albedo method has a unique advantage in DRFEdust estimation: it could validate the results derived from the numerical model directly.
Ruibo Lei, Mario Hoppmann, Bin Cheng, Guangyu Zuo, Dawei Gui, Qiongqiong Cai, H. Jakob Belter, and Wangxiao Yang
The Cryosphere, 15, 1321–1341, https://doi.org/10.5194/tc-15-1321-2021, https://doi.org/10.5194/tc-15-1321-2021, 2021
Short summary
Short summary
Quantification of ice deformation is useful for understanding of the role of ice dynamics in climate change. Using data of 32 buoys, we characterized spatiotemporal variations in ice kinematics and deformation in the Pacific sector of Arctic Ocean for autumn–winter 2018/19. Sea ice in the south and west has stronger mobility than in the east and north, which weakens from autumn to winter. An enhanced Arctic dipole and weakened Beaufort Gyre in winter lead to an obvious turning of ice drifting.
Y. Chen, X. Zhao, M. Qu, Z. Cheng, X. Pang, and Q. Ji
Int. Arch. Photogramm. Remote Sens. Spatial Inf. Sci., XLIII-B3-2020, 861–867, https://doi.org/10.5194/isprs-archives-XLIII-B3-2020-861-2020, https://doi.org/10.5194/isprs-archives-XLIII-B3-2020-861-2020, 2020
Thomas Krumpen, Florent Birrien, Frank Kauker, Thomas Rackow, Luisa von Albedyll, Michael Angelopoulos, H. Jakob Belter, Vladimir Bessonov, Ellen Damm, Klaus Dethloff, Jari Haapala, Christian Haas, Carolynn Harris, Stefan Hendricks, Jens Hoelemann, Mario Hoppmann, Lars Kaleschke, Michael Karcher, Nikolai Kolabutin, Ruibo Lei, Josefine Lenz, Anne Morgenstern, Marcel Nicolaus, Uwe Nixdorf, Tomash Petrovsky, Benjamin Rabe, Lasse Rabenstein, Markus Rex, Robert Ricker, Jan Rohde, Egor Shimanchuk, Suman Singha, Vasily Smolyanitsky, Vladimir Sokolov, Tim Stanton, Anna Timofeeva, Michel Tsamados, and Daniel Watkins
The Cryosphere, 14, 2173–2187, https://doi.org/10.5194/tc-14-2173-2020, https://doi.org/10.5194/tc-14-2173-2020, 2020
Short summary
Short summary
In October 2019 the research vessel Polarstern was moored to an ice floe in order to travel with it on the 1-year-long MOSAiC journey through the Arctic. Here we provide historical context of the floe's evolution and initial state for upcoming studies. We show that the ice encountered on site was exceptionally thin and was formed on the shallow Siberian shelf. The analyses presented provide the initial state for the analysis and interpretation of upcoming biogeochemical and ecological studies.
Jianwei Yang, Lingmei Jiang, Kari Luojus, Jinmei Pan, Juha Lemmetyinen, Matias Takala, and Shengli Wu
The Cryosphere, 14, 1763–1778, https://doi.org/10.5194/tc-14-1763-2020, https://doi.org/10.5194/tc-14-1763-2020, 2020
Short summary
Short summary
There are many challenges for accurate snow depth estimation using passive microwave data. Machine learning (ML) techniques are deemed to be powerful tools for establishing nonlinear relations between independent variables and a given target variable. In this study, we investigate the potential capability of the random forest (RF) model on snow depth estimation at temporal and spatial scales. The result indicates that the fitted RF algorithms perform better on temporal than spatial scales.
Dawei Gui, Xiaoping Pang, Ruibo Lei, Xi Zhao, and Jia Wang
Abstr. Int. Cartogr. Assoc., 1, 101, https://doi.org/10.5194/ica-abs-1-101-2019, https://doi.org/10.5194/ica-abs-1-101-2019, 2019
Haiyan Liu and Xiaoping Pang
Abstr. Int. Cartogr. Assoc., 1, 221, https://doi.org/10.5194/ica-abs-1-221-2019, https://doi.org/10.5194/ica-abs-1-221-2019, 2019
Xiaoping Pang, Pei Fan, Xi Zhao, and Qing Ji
Abstr. Int. Cartogr. Assoc., 1, 289, https://doi.org/10.5194/ica-abs-1-289-2019, https://doi.org/10.5194/ica-abs-1-289-2019, 2019
Meng Qu, Xiaoping Pang, Xi Zhao, Jinlun Zhang, Qing Ji, and Pei Fan
The Cryosphere, 13, 1565–1582, https://doi.org/10.5194/tc-13-1565-2019, https://doi.org/10.5194/tc-13-1565-2019, 2019
Short summary
Short summary
Can we ignore the contribution of small ice leads when estimating turbulent heat flux? Combining bulk formulae and a fetch-limited model with surface temperature from MODIS and Landsat-8 Thermal Infrared Sensor (TIRS) images, we found small leads account for 25 % of the turbulent heat flux, due to its large total area. Estimated turbulent heat flux is larger from TIRS than that from MODIS with a coarser resolution and larger using a fetch-limited model than that using bulk formulae.
Mi Liao, Sean Healy, and Peng Zhang
Atmos. Meas. Tech., 12, 2679–2692, https://doi.org/10.5194/amt-12-2679-2019, https://doi.org/10.5194/amt-12-2679-2019, 2019
Short summary
Short summary
This paper describes a new method for improving the data of the Chinese radio occultation sounder, GNOS, which has large biases. The new method can effectively eliminate about 90 % of the large departures. In addition, this paper also describes the quality control (QC) for the GNOS data. The GNOS data with the new L2 extrapolation are suitable for assimilation into numerical weather prediction systems.
Mi Liao, Peng Zhang, Guang-Lin Yang, Yan-Meng Bi, Yan Liu, Wei-Hua Bai, Xiang-Guang Meng, Qi-Fei Du, and Yue-Qiang Sun
Atmos. Meas. Tech., 9, 781–792, https://doi.org/10.5194/amt-9-781-2016, https://doi.org/10.5194/amt-9-781-2016, 2016
Short summary
Short summary
This paper provides a preliminary validation for the refractivity of GNOS, a new addition to the space-based radio occultation sounder on FY-3C. It possesses a similar sounding capability that COSMIC and GRAS did in the vertical range of 0-30 km, with a precision below 1 %.
W. H. Bai, Y. Q. Sun, Q. F. Du, G. L. Yang, Z. D. Yang, P. Zhang, Y. M. Bi, X. Y. Wang, C. Cheng, and Y. Han
Atmos. Meas. Tech., 7, 1817–1823, https://doi.org/10.5194/amt-7-1817-2014, https://doi.org/10.5194/amt-7-1817-2014, 2014
Related subject area
Domain: ESSD – Ice | Subject: Snow and Sea Ice
Time series of alpine snow surface radiative-temperature maps from high-precision thermal-infrared imaging
Operational and experimental snow observation systems in the upper Rofental: data from 2017 to 2023
A sea ice deformation and rotation rates dataset (2017–2023) from the Environment and Climate Change Canada Automated Sea Ice Tracking System (ECCC-ASITS)
An Arctic sea ice concentration data record on a 6.25 km polar stereographic grid from three-years’ Landsat-8 imagery
SMOS-derived Antarctic thin sea ice thickness: data description and validation in the Weddell Sea
A 12-year climate record of wintertime wave-affected marginal ice zones in the Atlantic Arctic based on CryoSat-2
MODIS daily cloud-gap-filled fractional snow cover dataset of the Asian Water Tower region (2000–2022)
Mapping of sea ice concentration using the NASA NIMBUS 5 Electrically Scanning Microwave Radiometer data from 1972–1977
A climate data record of year-round global sea-ice drift from the EUMETSAT Ocean and Sea Ice Satellite Application Facility (OSI SAF)
Snow accumulation and ablation measurements in a midlatitude mountain coniferous forest (Col de Porte, France, 1325 m altitude): the Snow Under Forest (SnoUF) field campaign data set
NH-SWE: Northern Hemisphere Snow Water Equivalent dataset based on in situ snow depth time series
IT-SNOW: a snow reanalysis for Italy blending modeling, in situ data, and satellite observations (2010–2021)
HMRFS–TP: long-term daily gap-free snow cover products over the Tibetan Plateau from 2002 to 2021 based on hidden Markov random field model
Sara Arioli, Ghislain Picard, Laurent Arnaud, Simon Gascoin, Esteban Alonso-González, Marine Poizat, and Mark Irvine
Earth Syst. Sci. Data, 16, 3913–3934, https://doi.org/10.5194/essd-16-3913-2024, https://doi.org/10.5194/essd-16-3913-2024, 2024
Short summary
Short summary
High-accuracy precision maps of the surface temperature of snow were acquired with an uncooled thermal-infrared camera during winter 2021–2022 and spring 2023. The accuracy – i.e., mean absolute error – improved from 1.28 K to 0.67 K between the seasons thanks to an improved camera setup and temperature stabilization. The dataset represents a major advance in the validation of satellite measurements and physical snow models over a complex topography.
Michael Warscher, Thomas Marke, Erwin Rottler, and Ulrich Strasser
Earth Syst. Sci. Data, 16, 3579–3599, https://doi.org/10.5194/essd-16-3579-2024, https://doi.org/10.5194/essd-16-3579-2024, 2024
Short summary
Short summary
Continuous observations of snow and climate at high altitudes are still sparse. We present a unique collection of weather and snow cover data from three automatic weather stations at remote locations in the Ötztal Alps (Austria) that include continuous recordings of snow cover properties. The data are available over multiple winter seasons and enable new insights for snow hydrological research. The data are also used in operational applications, i.e., for avalanche warning and flood forecasting.
Mathieu Plante, Jean-François Lemieux, L. Bruno Tremblay, Amélie Bouchat, Damien Ringeisen, Philippe Blain, Stephen Howell, Mike Brady, Alexander S. Komarov, Béatrice Duval, and Lekima Yakuden
Earth Syst. Sci. Data Discuss., https://doi.org/10.5194/essd-2024-227, https://doi.org/10.5194/essd-2024-227, 2024
Revised manuscript accepted for ESSD
Short summary
Short summary
Sea ice forms a thin boundary between the ocean and the atmosphere, with a complex crust-like dynamics and ever-changing networks of sea ice leads and ridges. Statistics of these dynamical features are often used to evaluate sea ice models. Here, we present a new pan-Arctic dataset of sea ice deformations derived from satellite imagery, from 01 September 2017 to 31 August 2023. We discuss the dataset coverage and some limitations associated with uncertainties in the computed values.
Hee-Sung Jung, Sang-Moo Lee, Joo-Hong Kim, and Kyungsoo Lee
Earth Syst. Sci. Data Discuss., https://doi.org/10.5194/essd-2024-264, https://doi.org/10.5194/essd-2024-264, 2024
Revised manuscript accepted for ESSD
Short summary
Short summary
This dataset consists of true-like sea ice concentration (SIC) data records over the Arctic Ocean, which was derived from the 30 m resolution imagery from the Operational Land Imager (OLI) onboard Landsat-8. Each SIC map are given in a 6.25 km polar stereographic grid, and are catalogued into one of the twelve sub-regions of the Arctic Ocean. This dataset was produced to be used as reference in validation of various SIC products.
Lars Kaleschke, Xiangshan Tian-Kunze, Stefan Hendricks, and Robert Ricker
Earth Syst. Sci. Data, 16, 3149–3170, https://doi.org/10.5194/essd-16-3149-2024, https://doi.org/10.5194/essd-16-3149-2024, 2024
Short summary
Short summary
We describe a sea ice thickness dataset based on SMOS satellite measurements, initially designed for the Arctic but adapted for Antarctica. We validated it using limited Antarctic measurements. Our findings show promising results, with a small difference in thickness estimation and a strong correlation with validation data within the valid thickness range. However, improvements and synergies with other sensors are needed, especially for sea ice thicker than 1 m.
Weixin Zhu, Siqi Liu, Shiming Xu, and Lu Zhou
Earth Syst. Sci. Data, 16, 2917–2940, https://doi.org/10.5194/essd-16-2917-2024, https://doi.org/10.5194/essd-16-2917-2024, 2024
Short summary
Short summary
In the polar ocean, wind waves generate and propagate into the sea ice cover, forming marginal ice zones (MIZs). Using ESA's CryoSat-2, we construct a 12-year dataset of the MIZ in the Atlantic Arctic, a key region for climate change and human activities. The dataset is validated with high-resolution observations by ICESat2 and Sentinel-1. MIZs over 300 km wide are found under storms in the Barents Sea. The new dataset serves as the basis for research areas, including wave–ice interactions.
Fangbo Pan, Lingmei Jiang, Gongxue Wang, Jinmei Pan, Jinyu Huang, Cheng Zhang, Huizhen Cui, Jianwei Yang, Zhaojun Zheng, Shengli Wu, and Jiancheng Shi
Earth Syst. Sci. Data, 16, 2501–2523, https://doi.org/10.5194/essd-16-2501-2024, https://doi.org/10.5194/essd-16-2501-2024, 2024
Short summary
Short summary
It is important to strengthen the continuous monitoring of snow cover as a key indicator of imbalance in the Asian Water Tower (AWT) region. We generate long-term daily gap-free fractional snow cover products over the AWT at 0.005° resolution from 2000 to 2022 based on the multiple-endmember spectral mixture analysis algorithm and the gap-filling algorithm. They can provide highly accurate, quantitative fractional snow cover information for subsequent studies on hydrology and climate.
Wiebke Margitta Kolbe, Rasmus T. Tonboe, and Julienne Stroeve
Earth Syst. Sci. Data, 16, 1247–1264, https://doi.org/10.5194/essd-16-1247-2024, https://doi.org/10.5194/essd-16-1247-2024, 2024
Short summary
Short summary
Current satellite-based sea-ice climate data records (CDRs) usually begin in October 1978 with the first multichannel microwave radiometer data. Here, we present a sea ice dataset based on the single-channel Electrical Scanning Microwave Radiometer (ESMR) that operated from 1972-1977 onboard NASA’s Nimbus 5 satellite. The data were processed using modern methods and include uncertainty estimations in order to provide an important, easy-to-use reference period of good quality for current CDRs.
Thomas Lavergne and Emily Down
Earth Syst. Sci. Data, 15, 5807–5834, https://doi.org/10.5194/essd-15-5807-2023, https://doi.org/10.5194/essd-15-5807-2023, 2023
Short summary
Short summary
Sea ice in the Arctic and Antarctic can move several tens of kilometers per day due to wind and ocean currents. By analysing thousands of satellite images, we measured how sea ice has been moving every single day from 1991 through to 2020. We compare our data to how buoys attached to the ice moved and find good agreement. Other scientists will now use our data to better understand if climate change has modified the way sea ice moves and in what way.
Jean Emmanuel Sicart, Victor Ramseyer, Ghislain Picard, Laurent Arnaud, Catherine Coulaud, Guilhem Freche, Damien Soubeyrand, Yves Lejeune, Marie Dumont, Isabelle Gouttevin, Erwan Le Gac, Frédéric Berger, Jean-Matthieu Monnet, Laurent Borgniet, Éric Mermin, Nick Rutter, Clare Webster, and Richard Essery
Earth Syst. Sci. Data, 15, 5121–5133, https://doi.org/10.5194/essd-15-5121-2023, https://doi.org/10.5194/essd-15-5121-2023, 2023
Short summary
Short summary
Forests strongly modify the accumulation, metamorphism and melting of snow in midlatitude and high-latitude regions. Two field campaigns during the winters 2016–17 and 2017–18 were conducted in a coniferous forest in the French Alps to study interactions between snow and vegetation. This paper presents the field site, instrumentation and collection methods. The observations include forest characteristics, meteorology, snow cover and snow interception by the canopy during precipitation events.
Adrià Fontrodona-Bach, Bettina Schaefli, Ross Woods, Adriaan J. Teuling, and Joshua R. Larsen
Earth Syst. Sci. Data, 15, 2577–2599, https://doi.org/10.5194/essd-15-2577-2023, https://doi.org/10.5194/essd-15-2577-2023, 2023
Short summary
Short summary
We provide a dataset of snow water equivalent, the depth of liquid water that results from melting a given depth of snow. The dataset contains 11 071 sites over the Northern Hemisphere, spans the period 1950–2022, and is based on daily observations of snow depth on the ground and a model. The dataset fills a lack of accessible historical ground snow data, and it can be used for a variety of applications such as the impact of climate change on global and regional snow and water resources.
Francesco Avanzi, Simone Gabellani, Fabio Delogu, Francesco Silvestro, Flavio Pignone, Giulia Bruno, Luca Pulvirenti, Giuseppe Squicciarino, Elisabetta Fiori, Lauro Rossi, Silvia Puca, Alexander Toniazzo, Pietro Giordano, Marco Falzacappa, Sara Ratto, Hervè Stevenin, Antonio Cardillo, Matteo Fioletti, Orietta Cazzuli, Edoardo Cremonese, Umberto Morra di Cella, and Luca Ferraris
Earth Syst. Sci. Data, 15, 639–660, https://doi.org/10.5194/essd-15-639-2023, https://doi.org/10.5194/essd-15-639-2023, 2023
Short summary
Short summary
Snow cover has profound implications for worldwide water supply and security, but knowledge of its amount and distribution across the landscape is still elusive. We present IT-SNOW, a reanalysis comprising daily maps of snow amount and distribution across Italy for 11 snow seasons from September 2010 to August 2021. The reanalysis was validated using satellite images and snow measurements and will provide highly needed data to manage snow water resources in a warming climate.
Yan Huang, Jiahui Xu, Jingyi Xu, Yelei Zhao, Bailang Yu, Hongxing Liu, Shujie Wang, Wanjia Xu, Jianping Wu, and Zhaojun Zheng
Earth Syst. Sci. Data, 14, 4445–4462, https://doi.org/10.5194/essd-14-4445-2022, https://doi.org/10.5194/essd-14-4445-2022, 2022
Short summary
Short summary
Reliable snow cover information is important for understating climate change and hydrological cycling. We generate long-term daily gap-free snow products over the Tibetan Plateau (TP) at 500 m resolution from 2002 to 2021 based on the hidden Markov random field model. The accuracy is 91.36 %, and is especially improved during snow transitional period and over complex terrains. This dataset has great potential to study climate change and to facilitate water resource management in the TP.
Cited articles
Arndt, S.: Sea ice conditions during POLARSTERN cruise PS111 (ANT-XXXIII/2,
FROST), Alfred Wegener Institute, Helmholtz Centre for Polar and Marine
Research, Bremerhaven, PANGAEA [data set], https://doi.org/10.1594/PANGAEA.887697,
2018.
Arndt, S.: Sea ice conditions during POLARSTERN cruise PS118 (LARSEN),
Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research,
Bremerhaven, PANGAEA [data set], https://doi.org/10.1594/PANGAEA.901263, 2019.
Arndt, S. and Castellani, G.: Sea ice conditions during POLARSTERN cruise
PS117, Alfred Wegener Institute, Helmholtz Centre for Polar and Marine
Research, Bremerhaven, PANGAEA [data set], https://doi.org/10.1594/PANGAEA.901279,
2019.
Arndt, S. and van Caspel, M.: Sea ice conditions during POLARSTERN cruise
PS103 (ANT-XXXII/2), Alfred Wegener Institute, Helmholtz Centre for Polar
and Marine Research, Bremerhaven, PANGAEA [data set],
https://doi.org/10.1594/PANGAEA.880046, 2017.
Beitsch, A., Kern, S., and Kaleschke, L.: Comparison of SSM/I and AMSR-E sea
ice concentrations with ASPeCt ship observations around Antarctica, IEEE
T. Geosci. Remote, 53, 1985–1996,
https://doi.org/10.1109/TGRS.2014.2351497, 2015.
Cavalieri, D. J., St. Germain, K. M., and Swift, C. T.: Reduction of weather
effects in the calculation of sea-ice concentration with the DMSP SSM/I, J.
Glaciol., 41, 455–464, https://doi.org/10.1017/S0022143000034791, 1995.
Cavalieri, D. J., Markus, T., and Comiso., J. C.: AMSR-E/Aqua Daily L3 12.5
km Brightness Temperature, Sea Ice Concentration, & Snow Depth Polar
Grids, Version 3, Boulder, Colorado USA, NASA National Snow and Ice Data
Center Distributed Active Archive Center [data set],
https://doi.org/10.5067/AMSR-E/AE_SI12.003, 2014.
Chen, Y., Zhao, X., Pang, X., and Ji, Q.: Daily sea ice concentration
product based on brightness temperature data of FY-3D MWRI in the Arctic,
Big Earth Data, 6, 164–178, https://doi.org/10.1080/20964471.2020.1865623,
2022a.
Chen, Y., Pang, X., Lei, R., and Zhao, X.: Sea ice concentration derived
from temperature brightness data of the Microwave Radiation Imager sensors
onboard the Chinese FengYun-3 satellites in the polar regions from 2010 to
2019, PANGAEA [data set], https://doi.org/10.1594/PANGAEA.945188, 2022b.
Comiso, J. C., Cavalieri, D. J., and Markus, T.: Sea ice concentration, ice
temperature, and snow depth using AMSR-E data, IEEE T. Geosci. Remote, 41, 243–252, https://doi.org/10.1109/TGRS.2002.808317, 2003.
Comiso, J. C., Meier, W. N., and Gersten, R.: Variability and trends in the
Arctic Sea ice cover: Results from different techniques, J. Geophys. Res.-Oceans, 122, 6883–6900, https://doi.org/10.1002/2017JC012768, 2017.
DiGirolamo, N. E., Parkinson C. L., Cavalieri, D. J., Gloersen, P., and Zwally, H. J.: Sea Ice
Concentrations from Nimbus-7 SMMR and DMSP SSM/I-SSMIS Passive Microwave
Data, Version 2, User Guide, National Snow and Ice Data Center, Boulder,
Colorado USA, p. 12, https://nsidc.org/sites/default/files/documents/user-guide/nsidc-0051-v002-userguide.pdf, last access: 17 July 2023.
Eisenman, I., Meier, W. N., and Norris, J. R.: A spurious jump in the satellite record: has Antarctic sea ice expansion been overestimated?, The Cryosphere, 8, 1289–1296, https://doi.org/10.5194/tc-8-1289-2014, 2014.
Esastar: Development and Commissioning of a CIMR Airborne Demonstrator (CIMR-AIR) – Expro+,
https://esastar-publication-ext.sso.esa.int/ESATenderActions/details/55123,
last access: 10 June 2023.
Fetterer, F., Knowles, K., Meier, W. N., Savoie, M. H., and Windnagel, A.
K.: Sea Ice Index, Version 3,
Boulder, Colorado USA, National Snow and Ice Data Center [data set],
https://doi.org/10.7265/N5K072F8, 2017.
Gerland, S., Barber, D., Meier, W., Mundy, C. J., Holland, M., Kern, S., Li,
Z., Michel, C., Perovich, D. K., and Tamura, T.: Essential gaps and
uncertainties in the understanding of the roles and functions of Arctic sea
ice, Environ. Res. Lett., 14, 043002, https://doi.org/10.1088/1748-9326/ab09b3,
2019.
Girard-Ardhuin, F., Ezraty, R., and Croizé-Fillon, D.: Arctic and
Antarctic sea ice concentration and sea ice drift satellite products at
Ifremer/CERSAT, Mercat. Ocean Q. Newsl., 34, 31–39, 2008.
Gloersen, P. and Cavalieri, D. J.: Reduction of weather effects in the
calculation of sea ice concentration from microwave radiances, J. Geophys.
Res.-Oceans, 91, 3913–3919, https://doi.org/10.1029/jc091ic03p03913, 1986.
Heil, P., Fowler, C. W., and Lake, S. E.: Antarctic sea-ice velocity as
derived from SSM/I imagery, Ann. Glaciol., 44, 361–366,
https://doi.org/10.3189/172756406781811682, 2006.
Hendricks, S., Nicolaus, M., and Schwegmann, S.: Sea ice conditions during
POLARSTERN cruise ARK-XXVII/3 (IceArc), Alfred Wegener Institute, Helmholtz
Centre for Polar and Marine Research, Bremerhaven, PANGAEA [data set],
https://doi.org/10.1594/PANGAEA.803221, 2012.
Hutchings, J., Delamere, J., and Heil, P.: The Ice Watch Manual, https://icewatch.met.no/Ice_Watch_Manual_v4.1.pdf (last access: 17 July 2023), 2020.
Ivanova, N., Pedersen, L. T., Tonboe, R. T., Kern, S., Heygster, G., Lavergne, T., Sørensen, A., Saldo, R., Dybkjær, G., Brucker, L., and Shokr, M.: Inter-comparison and evaluation of sea ice algorithms: towards further identification of challenges and optimal approach using passive microwave observations, The Cryosphere, 9, 1797–1817, https://doi.org/10.5194/tc-9-1797-2015, 2015.
Jiménez, C., Tenerelli, J., Prigent, C., Kilic, L., Lavergne, T.,
Skarpalezos, S., Høyer, J. L., Reul, N., and Donlon, C.: Ocean and Sea
Ice Retrievals From an End-To-End Simulation of the Copernicus Imaging
Microwave Radiometer (CIMR) 1.4–36.5 GHz Measurements, J. Geophys. Res.-Oceans, 126, e2021JC017610, https://doi.org/10.1029/2021JC017610, 2021.
Kaleschke, L., Lüpkes, C., Vihma, T., Haarpaintner, J., Bochert, A.,
Hartmann, J., and Heygster, G.: SSM/I sea ice remote sensing for mesoscale
ocean-atmosphere interaction analysis, Can. J. Remote Sens., 27, 526–537,
https://doi.org/10.1080/07038992.2001.10854892, 2001.
Katlein, C., Arndt, S., and Nicolaus, M.: Sea ice conditions during
POLARSTERN cruise PS86 (ARK-XXVIII/3 AURORA), Alfred Wegener Institute,
Helmholtz Centre for Polar and Marine Research, Bremerhaven, PANGAEA [data set],
https://doi.org/10.1594/PANGAEA.835578, 2014.
Kern, S.: A new method for medium-resolution sea ice analysis using
weather-influence corrected Special Sensor Microwave/Imager 85 GHz data,
Int. J. Remote Sens., 25, 4555–4582,
https://doi.org/10.1080/01431160410001698898, 2004.
Kern, S.: ESA-CCI_Phase2_Standardized_ Manual_Visual_Ship-Based_SeaIceObservations_v02, World Data
Center for Climate (WDCC) at DKRZ [data set],
https://doi.org/10.26050/WDCC/ESACCIPSMVSBSIOV2, 2020.
Kern, S., Rösel, A., Pedersen, L. T., Ivanova, N., Saldo, R., and Tonboe, R. T.: The impact of melt ponds on summertime microwave brightness temperatures and sea-ice concentrations, The Cryosphere, 10, 2217–2239, https://doi.org/10.5194/tc-10-2217-2016, 2016.
Kern, S., Lavergne, T., Notz, D., Pedersen, L. T., Tonboe, R. T., Saldo, R., and Sørensen, A. M.: Satellite passive microwave sea-ice concentration data set intercomparison: closed ice and ship-based observations, The Cryosphere, 13, 3261–3307, https://doi.org/10.5194/tc-13-3261-2019, 2019.
Kern, S., Kaleschke, L., Girard-Ardhuin, F., Spreen, G., and Beitsch, A.:
Global daily gridded 5-day median-filtered, gap-filled ASI Algorithm
SSMI-SSMIS sea ice concentration data, Integrated Climate Date Center
(ICDC), CEN, University of Hamburg, Germany [data set],
https://www.cen.uni-hamburg.de/en/icdc/data/cryosphere/seaiceconcentration-asi-ssmi.html (last access: 28 May 2022),
2023.
Lavergne, T., Sørensen, A. M., Kern, S., Tonboe, R., Notz, D., Aaboe, S., Bell, L., Dybkjær, G., Eastwood, S., Gabarro, C., Heygster, G., Killie, M. A., Brandt Kreiner, M., Lavelle, J., Saldo, R., Sandven, S., and Pedersen, L. T.: Version 2 of the EUMETSAT OSI SAF and ESA CCI sea-ice concentration climate data records, The Cryosphere, 13, 49–78, https://doi.org/10.5194/tc-13-49-2019, 2019.
Lavergne, T., Aaboe, S., Neuville, A., Sørensen, A., and
Eastwood, S.: Product User Manual for the Sea Ice Index, version 2.1, 18 pp., https://osisaf-hl.met.no/sites/osisaf-hl/files/user_manuals/osisaf_cdop3_ss2_pum_sea-ice-index_v1p0.pdf (last access: 17 July 2023),
2020.
Lavergne, T., Kern, S., Aaboe, S., Derby, L., Dybkjaer, G., Garric, G.,
Heil, P., Hendricks, S., Holfort, J., Howell, S., Key, J., Lieser, J. L.,
Maksym, T., Maslowski, W., Meier, W., Munoz-Sabater, J., Nicolas, J.,
Özsoy, B., Rabe, B., Rack, W., Raphael, M., de Rosnay, P., Smolyanitsky,
V., Tietsche, S., Ukita, J., Vichi, M., Wagner, P., Willmes, S., and Zhao,
X.: A New Structure for the Sea Ice Essential Climate Variables of the
Global Climate Observing System, B. Am. Meteorol. Soc., 103, E1502–E1521,
https://doi.org/10.1175/bams-d-21-0227.1, 2022.
Lei, R., Tian-Kunze, X., Li, B., Heil, P., Wang, J., Zeng, J., and Tian, Z.:
Characterization of summer Arctic sea ice morphology in the 135∘–175∘ W sector using multi-scale methods, Cold Reg. Sci. Technol.,
133, 108–120, https://doi.org/10.1016/j.coldregions.2016.10.009, 2017.
Li, N., Lei, R., Heil, P., Cheng, B., Ding, M., Tian, Z., and Li, B.: Seasonal and interannual variability of the landfast ice mass balance between 2009 and 2018 in Prydz Bay, East Antarctica, The Cryosphere, 17, 917–937, https://doi.org/10.5194/tc-17-917-2023, 2023.
Maaß, N. and Kaleschke, L.: Improving passive microwave sea ice
concentration algorithms for coastal areas: Applications to the Baltic Sea,
Tellus A: Dynamic Meteorology and Oceanography, 62, 393–410,
https://doi.org/10.1111/j.1600-0870.2010.00452.x, 2010.
Markus, T., Stroeve, J. C., and Miller, J.: Recent changes in Arctic sea ice
melt onset, freezeup, and melt season length, J. Geophys. Res.-Oceans, 114,
C12024, https://doi.org/10.1029/2009JC005436, 2009.
Maslanik, J. A., Serreze, M. C., and Barry, R. G.: Recent decreases in
Arctic summer ice cover and linkages to atmospheric circulation anomalies,
Geophys. Res. Lett., 23, 1677–1680, https://doi.org/10.1029/96GL01426,
1996.
Meier, W. N.: Satellite passive microwave observations of sea ice, 3rd edn., vol. 5, Encyclopedia of Ocean Sciences, 402–414, https://doi.org/10.1016/B978-0-12-409548-9.11461-7,
2019.
Meier, W. N. and Ivanoff, A.: Intercalibration of AMSR2 NASA Team 2
Algorithm Sea Ice Concentrations with AMSR-E Slow Rotation Data, IEEE J.
Sel. Top. Appl., 10, 3923–3933,
https://doi.org/10.1109/JSTARS.2017.2719624, 2017.
Meier, W. N. and Stewart, J. S.: Assessing uncertainties in sea ice extent
climate indicators, Environ. Res. Lett., 14, 035005,
https://doi.org/10.1088/1748-9326/aaf52c, 2019.
Meier, W. N., Markus, T., and Comiso, J. C.: AMSR-E/AMSR2 Unified L3 Daily
12.5 km Brightness Temperatures, Sea Ice Concentration, Motion & Snow
Depth Polar Grids, Version 1, Boulder, Colorado USA, NASA National Snow and
Ice Data Center Distributed Active Archive Center [data set],
https://doi.org/10.5067/RA1MIJOYPK3P, 2018.
Meier, W. N., Stewart, J. S., Wilcox, H., Scott, D. J., and Hardman, M. A.:
DMSP SSM/I-SSMIS Daily Polar Gridded Brightness Temperatures, Version 6,
Boulder, Colorado USA, NASA National Snow and Ice Data Center Distributed
Active Archive Center [data set], https://doi.org/10.5067/MXJL42WSXTS1, 2021.
Melsheimer, C. and Spreen, G.: AMSR-E/AMSR2 ASI sea ice concentration data,
Arctic and Antarctic, version 5.4, Institute of Environmental Physics, University of Bremen, Germany [data set], https://data.seaice.uni-bremen.de/ (last access: 28 May 2022), 2023.
Newell, D., Draper, D., Remund, Q., Woods, B., Mays, C., Bensler, B.,
Miller, D., and Eastman, K.: Weather Satellite Follow-On – Microwave (WSF-M)
design and predicted performance, Ball Aerospace, Boulder, Colorado, USA, https://ams.confex.com/ams/2020Annual/webprogram/Manuscript/Paper369912/WSFM AMS Final.pdf (last access: 17 July 2023),
2020.
Parkinson, C. L. and DiGirolamo, N. E.: Sea ice extents continue to set new
records: Arctic, Antarctic, and global results, Remote Sens. Environ., 267,
112753, https://doi.org/10.1016/j.rse.2021.112753, 2021.
Spreen, G., Kaleschke, L., and Heygster, G.: Sea ice remote sensing using
AMSR-E 89-GHz channels, J. Geophys. Res.-Oceans, 113, C02S03,
https://doi.org/10.1029/2005JC003384, 2008.
Stroeve, J. and Meier, W. N.: Sea Ice Trends and Climatologies from SMMR and
SSM/I-SSMIS, Version 3 [Monthly total Sea Ice Extent], Boulder, Colorado
USA, NASA National Snow and Ice Data Center Distributed Active Archive
Center [data set], https://doi.org/10.5067/IJ0T7HFHB9Y6, 2018.
Svendsen, E., Matzler, C., and Grenfell, T. C.: A model for retrieving total
sea ice concentration from a spaceborne dual-polarized passive microwave
instrument operating near 90 GHz, Int. J. Remote Sens., 8, 1479–1487,
https://doi.org/10.1080/01431168708954790, 1987.
Trewin, B., Cazenave, A., Howell, S., Huss, M., Isensee, K., Palmer, M. D.,
Tarasova, O., and Vermeulen, A.: Headline indicators for global climate
monitoring, B. Am. Meteorol. Soc., 102, E20–E37,
https://doi.org/10.1175/BAMS-D-19-0196.1, 2021.
Worby, A. P. and Allison, I.: A technique for making ship-based observations of Antarctic sea ice thickness and characteristics. Part I. Observational techniques and results, https://www.researchgate.net/publication/292603529 (last access: 17 July 2023), 1999.
Wu, S. and Liu, J.: Comparison of Arctic sea ice concentration datasets,
Acta Ocean. Sin, 40, 64–72,
https://doi.org/10.3969/j.issn.0253-4193.2018.11.007, 2018.
Xian, D., Zhang, P., Gao, L., Sun, R., Zhang, H., and Jia, X.: Fengyun
Meteorological Satellite Products for Earth System Science Applications,
Adv. Atmos. Sci., 38, 1267–1284, https://doi.org/10.1007/s00376-021-0425-3,
2021.
Xie, H., Lei, R., Ke, C., Wang, H., Li, Z., Zhao, J., and Ackley, S. F.: Summer sea ice characteristics and morphology in the Pacific Arctic sector as observed during the CHINARE 2010 cruise, The Cryosphere, 7, 1057–1072, https://doi.org/10.5194/tc-7-1057-2013, 2013.
Zhang, P., Chen, L., Xian, D., Zhe, X., Peng, Z., Lin, C., and Di, X.:
Recent progress of Fengyun meteorology satellites, Chin. J. Sp. Sci, 38,
788–796, https://doi.org/10.11728/cjss2018.05.788, 2018.
Zhang, P., Lu, Q., Hu, X., Gu, S., Yang, L., Min, M., Chen, L., Xu, N., Sun,
L., Bai, W., Ma, G., and Xian, D.: Latest Progress of the Chinese
Meteorological Satellite Program and Core Data Processing Technologies, Adv.
Atmos. Sci., 36, 1027–1045, https://doi.org/10.1007/s00376-019-8215-x,
2019.
Zhao, X., Chen, Y., Kern, S., Qu, M., Ji, Q., Fan, P., and Liu, Y.: Sea Ice
Concentration Derived from FY-3D MWRI and Its Accuracy Assessment, IEEE
T. Geosci. Remote, 60, 4300418, https://doi.org/10.1109/TGRS.2021.3063272,
2022.
Short summary
The sea ice concentration product derived from the Microwave Radiation Image sensors on board the FengYun-3 satellites can reasonably and independently identify the seasonal and long-term changes of sea ice, as well as extreme cases of annual maximum and minimum sea ice extent in polar regions. It is comparable with other sea ice concentration products and applied to the studies of climate and marine environment.
The sea ice concentration product derived from the Microwave Radiation Image sensors on board...
Altmetrics
Final-revised paper
Preprint