{
    "created": "2026-05-31 16:13:42",
    "updated": "2026-06-01 05:37:00",
    "id": "7ec1c65b-17ee-412a-a535-135aa758a97a",
    "version": 6,
    "ds_topic": null,
    "title_cn": "北半球多年冻土区冬季CO₂排放数据集(1982-2022年)",
    "title_en": "A dataset of winter CO₂ emissions in the Northern Hemisphere permafrost regions from 1982 to 2022",
    "ds_abstract": "<p>&emsp;&emsp;气候变暖正加速多年冻土有机碳分解，尤其是在冬季时期。然而由于缺乏高质量与网格化的冬季CO₂排放时序数据，目前对北半球多年冻土区冬季CO₂排放的评估存在较大的不确定性。本研究构建了北半球多年冻土区1982-2022年0.1°空间分辨率的冬季CO₂通量数据集。该数据集整合了2487个月度冬季CO₂通量观测数据和多源地理空间数据，包括气候、植被、积雪、土壤及多年冻土，基于极端随机树模型对北极和青藏高原分别建模升尺度冬季CO₂通量生成。验证结果表明模型性能良好，在北极多年冻土区的R²为0.67，MAE和RMSE分别为3.94 g C m⁻² month⁻¹与5.67 g C m⁻² month⁻¹，而在青藏高原的R²为0.82，MAE和RMSE分别为2.76 g C m⁻² month⁻¹与3.76 g C m⁻² month⁻¹。该数据可为多年冻土区生态系统碳循环研究提供基础数据支持。",
    "ds_source": "",
    "ds_process_way": "",
    "ds_quality": "",
    "ds_acq_start_time": null,
    "ds_acq_end_time": null,
    "ds_acq_place": "",
    "ds_acq_lon_east": 180.0,
    "ds_acq_lat_south": 27.07,
    "ds_acq_lon_west": -180.0,
    "ds_acq_lat_north": 83.67,
    "ds_acq_alt_low": null,
    "ds_acq_alt_high": null,
    "ds_share_type": "apply-access",
    "ds_total_size": 334928273,
    "ds_files_count": 0,
    "ds_format": "*.tif",
    "ds_space_res": "0.1°",
    "ds_time_res": "年",
    "ds_coordinate": "无",
    "ds_projection": "",
    "ds_thumbnail": "8414b6e3-51a1-40fb-931b-3dc10041ae47.jpg",
    "ds_thumb_from": 0,
    "ds_ref_way": "",
    "paper_ref_way": "",
    "ds_ref_instruction": "",
    "ds_from_station": null,
    "organization_id": "52b7b79b-860c-49a5-9083-9a70cf8bed5a",
    "ds_serv_man": null,
    "ds_serv_phone": null,
    "ds_serv_mail": null,
    "doi_value": "",
    "subject_codes": [
        "170.45",
        "170.4510"
    ],
    "quality_level": 0,
    "publish_time": "2026-06-01 09:54:05",
    "last_updated": "2026-06-01 10:02:58",
    "protected": false,
    "protected_to": null,
    "lang": "zh",
    "cstr": "11738.11.ncdc.permafrost.db7432.2026",
    "i18n": {
        "en": {
            "title": "A dataset of winter CO₂ emissions in the Northern Hemisphere permafrost regions from 1982 to 2022",
            "ds_format": "*.tif",
            "ds_source": "",
            "ds_quality": "",
            "ds_ref_way": "",
            "ds_abstract": "<p>&emsp;Global warming is accelerating the decomposition of organic carbon stored in permafrost regions, particularly during winter when photosynthesis ceases. However, due to the lack of high-quality and gridded time-series data on winter CO₂ fluxes, substantial uncertainty remains in assessing winter CO₂ emissions across the Northern Hemisphere permafrost regions. This study constructed a dataset of winter CO₂ flux at a spatial resolution of 0.1° for Northern Hemisphere permafrost regions from 1982 to 2022. The dataset integrates 2,487 monthly winter CO₂ flux observations with multi-source geospatial data, including climate, vegetation, snow cover, soil properties, and permafrost characteristics. Winter CO₂ fluxes were upscaled separately for the Arctic and the Tibetan Plateau using an Extremely Randomized Trees model. Validation results indicate excellent model performance, with an R² of 0.67, an MAE of 3.94 g C m⁻² month⁻¹, and an RMSE of 5.67 g C m⁻² month⁻¹ for the Arctic permafrost region; and an R² of 0.82, an MAE of 2.76 g C m⁻² month⁻¹, and an RMSE of 3.76 g C m⁻² month⁻¹ for the Tibetan Plateau. This dataset provides fundamental support for research on carbon cycling in permafrost ecosystems.",
            "ds_time_res": "",
            "ds_acq_place": "",
            "ds_space_res": "",
            "ds_projection": "",
            "ds_process_way": "",
            "ds_ref_instruction": ""
        }
    },
    "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": [
        "北极",
        "青藏高原",
        "多年冻土",
        "气候变化",
        "冬季CO₂排放"
    ],
    "ds_subject_tags": [
        "地理学",
        "自然地理学"
    ],
    "ds_class_tags": [],
    "ds_locus_tags": [
        "北半球",
        "北极",
        "青藏高原",
        "多年冻土区"
    ],
    "ds_time_tags": [
        1982,
        1983,
        1984,
        1985,
        1986,
        1987,
        1988,
        1989,
        1990,
        1991,
        1992,
        1993,
        1994,
        1995,
        1996,
        1997,
        1998,
        1999,
        2000,
        2001,
        2002,
        2003,
        2004,
        2005,
        2006,
        2007,
        2008,
        2009,
        2010,
        2011,
        2012,
        2013,
        2014,
        2015,
        2016,
        2017,
        2018,
        2019,
        2020,
        2021,
        2022
    ],
    "ds_contributors": [
        {
            "true_name": "牟翠翠",
            "email": "mucc@lzu.edu.cn",
            "work_for": "兰州大学资源环境学院西部环境教育部重点实验室",
            "country": "中国"
        },
        {
            "true_name": "魏玉国",
            "email": "weiyg2024@lzu.edu.cn",
            "work_for": "兰州大学",
            "country": "中国"
        }
    ],
    "ds_meta_authors": [
        {
            "true_name": "牟翠翠",
            "email": "mucc@lzu.edu.cn",
            "work_for": "兰州大学资源环境学院西部环境教育部重点实验室",
            "country": "中国"
        },
        {
            "true_name": "魏玉国",
            "email": "weiyg2024@lzu.edu.cn",
            "work_for": "兰州大学",
            "country": "中国"
        }
    ],
    "ds_managers": [
        {
            "true_name": "牟翠翠",
            "email": "mucc@lzu.edu.cn",
            "work_for": "兰州大学资源环境学院西部环境教育部重点实验室",
            "country": "中国"
        }
    ],
    "category": "冻土"
}