{
    "created": "2026-06-18 09:26:37",
    "updated": "2026-06-18 08:23:40",
    "id": "891af79c-7c85-4854-bbf8-aa64e6b657d8",
    "version": 4,
    "ds_topic": null,
    "title_cn": "全球首套基于SMOS单角度信息的土壤水分、植被光学厚度与40°重建亮温数据集（2010-2024 年）",
    "title_en": "An operational global L-band soil moisture and vegetation optical depth dataset from optimized 40° SMOS brightness temperatures",
    "ds_abstract": "<p>&emsp;&emsp;本数据集提供逐日 SMOS-IB 亮温（TB）、土壤水分（SM）与植被光学深度（VOD）产品。该数据集基于 SMOS 卫星观测数据，依托 L-MEB 辐射传输模型重构得到降噪后的 40° 单角度亮温序列。优化后的 40° 亮温与 SMAP 卫星观测几何保持一致，大幅削弱了法国土壤湿度数据中心（CATDS）多角度 SMOS 三级亮温产品中存在的高频噪声。\n<p>&emsp;&emsp;研究采用 SMAP-INRAE-BORDEAUX（SMAP-IB）反演算法，并结合更新后的地表粗糙度数据集，生成 SMOS-IB 土壤水分与植被光学深度产品（Li 等，2022；Konkathi 等，2025）。将该产品与国际土壤水分网络（ISMN）实测土壤水分、多类植被代用指标开展对比验证，结果表明其精度优于多角度 SMOS 标准产品。数据集时间跨度为 2010-2024 年，空间分辨率 25 km，提供全球逐日 40° 入射角亮温、土壤水分及植被光学深度数据，适用于 L 波段反演算法开发、SMAP 数据一致性同化、全球干旱监测，以及植被水分与生物量动态相关研究。\n<p>&emsp;&emsp;开展各类应用分析或精度验证前，需对数据进行严格质量控制。数据筛选仅需借助场景标识层（Scene_Flags，简写 SF）与均方根误差层（RMSE）两类栅格。\n<p>&emsp;&emsp;筛选步骤如下：\n<p>&emsp;&emsp;1.采用条件 SF ≤ 1 过滤逐日土壤水分 / 植被光学深度数据，剔除地形干扰严重、地表冻结及无线电污染区域的无效像元；\n<p>&emsp;&emsp;2.设定亮温均方根误差阈值 TB-RMSE ≤ 8 K 或 TB-RMSE ≤ 6 K，去除强射频干扰（RFI）像元。该阈值可按需调整：阈值过大会降低土壤水分、植被光学深度数据质量；阈值过小则会过滤掉大量有效逐日观测样本。阈值选择需结合研究目标，全球尺度验证研究通常选用 6 K 或 8 K。\n<p>&emsp;&emsp;所有数据采用 netCDF4 格式存储，变量为 64 位双精度浮点型；空间网格采用全球第二代等面积可扩展地球网格（EASE-Grid 2.0），空间分辨率 25 千米。单个文件栅格尺寸为 584 行 ×1388 列。\n<p>&emsp;&emsp;注意事项\n<p>&emsp;&emsp;1.植被光学深度（VOD）正常取值范围为 [0, 2]，土壤水分（SM）正常取值范围为 [0, 1]；\n<p>&emsp;&emsp;2.部分区域年中值 VOD/SM 出现负值，该类数值无物理意义，已统一赋值为 0（异常像元主要分布于撒哈拉沙漠与澳大利亚中部）。",
    "ds_source": "",
    "ds_process_way": "",
    "ds_quality": "",
    "ds_acq_start_time": "2010-01-01 00:00:00",
    "ds_acq_end_time": "2024-12-31 00:00:00",
    "ds_acq_place": "全球",
    "ds_acq_lon_east": null,
    "ds_acq_lat_south": null,
    "ds_acq_lon_west": null,
    "ds_acq_lat_north": null,
    "ds_acq_alt_low": null,
    "ds_acq_alt_high": null,
    "ds_share_type": "open-access",
    "ds_total_size": 13884686464,
    "ds_files_count": 0,
    "ds_format": "NetCDF4",
    "ds_space_res": "25km",
    "ds_time_res": "日",
    "ds_coordinate": "无",
    "ds_projection": "",
    "ds_thumbnail": "891af79c-7c85-4854-bbf8-aa64e6b657d8.png",
    "ds_thumb_from": 0,
    "ds_ref_way": "",
    "paper_ref_way": "",
    "ds_ref_instruction": "使用 SMOS-IB 数据集必须引用以下文献：\r\n1.Xing et al., 2025. An operational global L-band soil moisture and vegetation optical depth dataset from optimized 40° SMOS brightness temperatures. ESSD. (In submission)\r\n2.Li, X., Wigneron, J. P., Frappart, F., De Lannoy, G., Fan, L., Zhao, T., ... & Ciais, P. (2022). The first global soil moisture and vegetation optical depth product retrieved from fused SMOS and SMAP L-band observations. Remote Sensing of Environment, 282, 113272.\r\n3.Li, X., Ciais, P. et al., Large live biomass carbon losses from droughts in the northern temperate ecosystems during 2016-2022. (2025). Nature Communications. https://doi.org/10.1038/s41467-025-59999-2",
    "ds_from_station": null,
    "organization_id": "0a4269e1-65f4-45f1-aeba-88ea3068eebf",
    "ds_serv_man": null,
    "ds_serv_phone": null,
    "ds_serv_mail": null,
    "doi_value": "",
    "subject_codes": [
        "170.2055",
        "170.45"
    ],
    "quality_level": 0,
    "publish_time": "2026-06-18 09:52:03",
    "last_updated": "2026-06-18 10:16:17",
    "protected": false,
    "protected_to": null,
    "lang": "zh",
    "cstr": "11738.11.ncdc.remote_sensing.db7456.2026",
    "i18n": {
        "en": {
            "title": "An operational global L-band soil moisture and vegetation optical depth dataset from optimized 40° SMOS brightness temperatures",
            "ds_format": "NetCDF4",
            "ds_source": "",
            "ds_quality": "",
            "ds_ref_way": "",
            "ds_abstract": "<p>&emsp;This repository provides daily SMOS-IB brightness temperature (TB), soil moisture (SM), and vegetation optical depth (VOD) products, derived from SMOS observations after reconstructing a noise-reduced 40° mono-angular TB record using the L-MEB radiative transfer model. The optimized 40° TB is consistent with the SMAP viewing geometry and substantially reduces the high-frequency noise present in the CATDS multi-angular SMOS Level-3 TB.\r\n<p>&emsp;SMOS-IB SM and VOD were then retrieved using the SMAP-INRAE-BORDEAUX (SMAP-IB) algorithm with updated soil roughness map (Li et al., 2022; Konkathi et al., 2025). Evaluations against ISMN soil moisture measurements and multiple vegetation proxies show improved performance compared with multi-angular SMOS products. The dataset provides global daily 40° TB, SM, and VOD at 25 km from 2010 to 2024, suitable for L-band algorithm development and SMAP harmonization, global drought monitoring, and studies of vegetation water and biomass dynamics.\r\n<p>&emsp;Before doing any application or validation studies, the quality control of the data should be done carefully. For the data filtering, we just need to use Scene_Flags (SF) and RMSE layers.\r\n<p>&emsp;Firstly, we usually filter the daily SM/VOD values by the conditions “SF <= 1” to remove the strong Topo, frozen scene and polluted scene. Then, we use TB-RMSE <= 8k or TB-RMSE <= 6k to remove strong RFI impact (this RMSE threshold can be higher or lower, but a higher value will reduce the quality of the SM/VOD, and a lower value will mask out too many daily observations; this value depends on your application, usually for global scale validation, we choose 6 or 8K).",
            "ds_time_res": "",
            "ds_acq_place": "global",
            "ds_space_res": "",
            "ds_projection": "",
            "ds_process_way": "",
            "ds_ref_instruction": "Citation of these papers is compulsory when you use the SMOS-IB product:\r\n1.Xing et al., 2025. An operational global L-band soil moisture and vegetation optical depth dataset from optimized 40° SMOS brightness temperatures. ESSD. (In submission)\r\n2.Li, X., Wigneron, J. P., Frappart, F., De Lannoy, G., Fan, L., Zhao, T., ... & Ciais, P. (2022). The first global soil moisture and vegetation optical depth product retrieved from fused SMOS and SMAP L-band observations. Remote Sensing of Environment, 282, 113272.\r\n3.Li, X., Ciais, P. et al., Large live biomass carbon losses from droughts in the northern temperate ecosystems during 2016-2022. (2025). Nature Communications. https://doi.org/10.1038/s41467-025-59999-2"
        }
    },
    "submit_center_id": "ncdc",
    "data_level": 0,
    "recommendation_value": 0,
    "license_type": "https://creativecommons.org/licenses/by/4.0/",
    "doi_reg_from": "reg_local",
    "cstr_reg_from": "reg_local",
    "doi_not_reg_reason": null,
    "cstr_not_reg_reason": null,
    "is_paper_in_submitting": false,
    "belong_to_nieer": false,
    "ds_topic_tags": [
        "亮温",
        "土壤水分",
        "植被光学深度"
    ],
    "ds_subject_tags": [
        "放射性地球物理学",
        "地理学"
    ],
    "ds_class_tags": [],
    "ds_locus_tags": [
        "全球"
    ],
    "ds_time_tags": [
        2010,
        2011,
        2012,
        2013,
        2014,
        2015,
        2016,
        2017,
        2018,
        2019,
        2020,
        2021,
        2022,
        2023,
        2024
    ],
    "ds_contributors": [
        {
            "true_name": "李小军",
            "email": "xiaojunli_vod@163.com",
            "work_for": "西南交通大学地球科学与工程学院",
            "country": "中国"
        }
    ],
    "ds_meta_authors": [
        {
            "true_name": "李小军",
            "email": "xiaojunli_vod@163.com",
            "work_for": "西南交通大学地球科学与工程学院",
            "country": "中国"
        }
    ],
    "ds_managers": [
        {
            "true_name": "李小军",
            "email": "xiaojunli_vod@163.com",
            "work_for": "西南交通大学地球科学与工程学院",
            "country": "中国"
        }
    ],
    "category": "遥感及产品"
}