{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2025,10,11]],"date-time":"2025-10-11T02:45:51Z","timestamp":1760150751993,"version":"build-2065373602"},"reference-count":43,"publisher":"MDPI AG","issue":"24","license":[{"start":{"date-parts":[[2023,12,14]],"date-time":"2023-12-14T00:00:00Z","timestamp":1702512000000},"content-version":"vor","delay-in-days":0,"URL":"https:\/\/creativecommons.org\/licenses\/by\/4.0\/"}],"funder":[{"name":"Science and Technology Development Fund, Institute of Desert Meteorology, China Meteorological Administration, Urumqi","award":["KJFZ202302","2023-38","IDM2021005","42305132","41875023","MS202312","ZD202306"],"award-info":[{"award-number":["KJFZ202302","2023-38","IDM2021005","42305132","41875023","MS202312","ZD202306"]}]},{"name":"Sandstorm laboratory project","award":["KJFZ202302","2023-38","IDM2021005","42305132","41875023","MS202312","ZD202306"],"award-info":[{"award-number":["KJFZ202302","2023-38","IDM2021005","42305132","41875023","MS202312","ZD202306"]}]},{"name":"Central Scientific Research Institute of the Public Basic Scientific Research Business Professional","award":["KJFZ202302","2023-38","IDM2021005","42305132","41875023","MS202312","ZD202306"],"award-info":[{"award-number":["KJFZ202302","2023-38","IDM2021005","42305132","41875023","MS202312","ZD202306"]}]},{"name":"National Natural Science Foundation of China","award":["KJFZ202302","2023-38","IDM2021005","42305132","41875023","MS202312","ZD202306"],"award-info":[{"award-number":["KJFZ202302","2023-38","IDM2021005","42305132","41875023","MS202312","ZD202306"]}]},{"name":"Science and technology innovation development Foundation of Xinjiang Meteorological Bureau","award":["KJFZ202302","2023-38","IDM2021005","42305132","41875023","MS202312","ZD202306"],"award-info":[{"award-number":["KJFZ202302","2023-38","IDM2021005","42305132","41875023","MS202312","ZD202306"]}]},{"name":"Innovation Team Project of Xinjiang Meteorological Service","award":["KJFZ202302","2023-38","IDM2021005","42305132","41875023","MS202312","ZD202306"],"award-info":[{"award-number":["KJFZ202302","2023-38","IDM2021005","42305132","41875023","MS202312","ZD202306"]}]}],"content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":["Remote Sensing"],"abstract":"<jats:p>Based on data from the Gurbantunggut Desert, the largest fixed\/semi-fixed desert in China, and ERA5-Land reanalysis data, the long-term variations and spatial surface heat source (SHS) differences in the Gurbantunggut Desert are discussed herein. The results show the following: (1) The hourly SHS at the Kelameili station during the 2013\u20132021 period was a weak heat source at night; contrastingly, it was a strong heat source during the day. The duration of the hourly SHS increased gradually from January to July, but it decreased gradually from July to December. The daily SHS showed obvious seasonal variation, reaching the maximum in summer and the minimum in winter. The ERA5-Land reanalysis can reproduce all the variation characteristics of the SHS well. (2) The climatology (i.e., multi-year mean) of the monthly SHS intensity was lower than 50 W\/m2 during the January\u2013March and September\u2013December periods in the Gurbantunggut Desert, indicating a weak heat source. On the other hand, the climatology recorded in April\u2013August was higher than 50 W\/m2, with a strong heat source. From the perspective of spatial distribution, the eastern and western regions of the Gurbantunggut Desert show strong heat sources, while the central region shows weak heat sources. The spatial distribution of the first and second modes of the empirical orthogonal function (EOF) decomposition reflected the consistent spatial variability and a north\u2013south (or east\u2013west) polarity variation of the monthly SHS in the Gurbantunggut Desert, respectively. (3) The yearly SHS showed negative anomalies during the 1950\u20131954, 1964\u20131982 and 2004\u20132015 periods, and positive anomalies during the 1955\u20131963, 1983\u20132003 and 2016\u20132021 periods in the Gurbantunggut Desert. Additionally, the time series of the SHS anomalies was positively correlated with the Interdecadal Pacific Oscillation (IPO) index. During the negative IPO phase, the yearly SHS showed a negative anomaly in the Gurbantunggut Desert, while the yearly SHS showed a positive anomaly during the positive IPO phase in most regions of the Gurbantunggut Desert.<\/jats:p>","DOI":"10.3390\/rs15245731","type":"journal-article","created":{"date-parts":[[2023,12,15]],"date-time":"2023-12-15T08:12:57Z","timestamp":1702627977000},"page":"5731","update-policy":"https:\/\/doi.org\/10.3390\/mdpi_crossmark_policy","source":"Crossref","is-referenced-by-count":2,"title":["Temporal and Spatial Surface Heat Source Variation in the Gurbantunggut Desert from 1950 to 2021"],"prefix":"10.3390","volume":"15","author":[{"given":"Ailiyaer","family":"Aihaiti","sequence":"first","affiliation":[{"name":"Institute of Desert Meteorology, China Meteorological Administration, Urumqi 830002, China"},{"name":"National Observation and Research Station of Desert Meteorology, Taklimakan Desert of Xinjiang, Urumqi 830002, China"},{"name":"Taklimakan Desert Meteorology Field Experiment Station of China Meteorological Administration, Urumqi 830002, China"},{"name":"Xinjiang Key Laboratory of Desert Meteorology and Sandstorm, Urumqi 830002, China"},{"name":"Key Laboratory of Tree-Ring Physical and Chemical Research, China Meteorological Administration, Urumqi 830002, China"}],"role":[{"role":"author","vocabulary":"crossref"}]},{"given":"Yu","family":"Wang","sequence":"additional","affiliation":[{"name":"Institute of Desert Meteorology, China Meteorological Administration, Urumqi 830002, China"},{"name":"National Observation and Research Station of Desert Meteorology, Taklimakan Desert of Xinjiang, Urumqi 830002, China"},{"name":"Taklimakan Desert Meteorology Field Experiment Station of China Meteorological Administration, Urumqi 830002, China"},{"name":"Xinjiang Key Laboratory of Desert Meteorology and Sandstorm, Urumqi 830002, China"},{"name":"Key Laboratory of Tree-Ring Physical and Chemical Research, China Meteorological Administration, Urumqi 830002, China"}],"role":[{"role":"author","vocabulary":"crossref"}]},{"ORCID":"https:\/\/orcid.org\/0000-0001-7335-801X","authenticated-orcid":false,"given":"Ali","family":"Mamtimin","sequence":"additional","affiliation":[{"name":"Institute of Desert Meteorology, China Meteorological Administration, Urumqi 830002, China"},{"name":"National Observation and Research Station of Desert Meteorology, Taklimakan Desert of Xinjiang, Urumqi 830002, China"},{"name":"Taklimakan Desert Meteorology Field Experiment Station of China Meteorological Administration, Urumqi 830002, China"},{"name":"Xinjiang Key Laboratory of Desert Meteorology and Sandstorm, Urumqi 830002, China"},{"name":"Key Laboratory of Tree-Ring Physical and Chemical Research, China Meteorological Administration, Urumqi 830002, China"}],"role":[{"role":"author","vocabulary":"crossref"}]},{"ORCID":"https:\/\/orcid.org\/0000-0002-8339-293X","authenticated-orcid":false,"given":"Junjian","family":"Liu","sequence":"additional","affiliation":[{"name":"Institute of Desert Meteorology, China Meteorological Administration, Urumqi 830002, China"},{"name":"National Observation and Research Station of Desert Meteorology, Taklimakan Desert of Xinjiang, Urumqi 830002, China"},{"name":"Taklimakan Desert Meteorology Field Experiment Station of China Meteorological Administration, Urumqi 830002, China"},{"name":"Xinjiang Key Laboratory of Desert Meteorology and Sandstorm, Urumqi 830002, China"},{"name":"Key Laboratory of Tree-Ring Physical and Chemical Research, China Meteorological Administration, Urumqi 830002, China"}],"role":[{"role":"author","vocabulary":"crossref"}]},{"given":"Jiacheng","family":"Gao","sequence":"additional","affiliation":[{"name":"Institute of Desert Meteorology, China Meteorological Administration, Urumqi 830002, China"},{"name":"National Observation and Research Station of Desert Meteorology, Taklimakan Desert of Xinjiang, Urumqi 830002, China"},{"name":"Taklimakan Desert Meteorology Field Experiment Station of China Meteorological Administration, Urumqi 830002, China"},{"name":"Xinjiang Key Laboratory of Desert Meteorology and Sandstorm, Urumqi 830002, China"},{"name":"Key Laboratory of Tree-Ring Physical and Chemical Research, China Meteorological Administration, Urumqi 830002, China"}],"role":[{"role":"author","vocabulary":"crossref"}]},{"given":"Meiqi","family":"Song","sequence":"additional","affiliation":[{"name":"Institute of Desert Meteorology, China Meteorological Administration, Urumqi 830002, China"},{"name":"National Observation and Research Station of Desert Meteorology, Taklimakan Desert of Xinjiang, Urumqi 830002, China"},{"name":"Taklimakan Desert Meteorology Field Experiment Station of China Meteorological Administration, Urumqi 830002, China"},{"name":"Xinjiang Key Laboratory of Desert Meteorology and Sandstorm, Urumqi 830002, China"},{"name":"Key Laboratory of Tree-Ring Physical and Chemical Research, China Meteorological Administration, Urumqi 830002, China"}],"role":[{"role":"author","vocabulary":"crossref"}]},{"ORCID":"https:\/\/orcid.org\/0009-0003-4871-4678","authenticated-orcid":false,"given":"Cong","family":"Wen","sequence":"additional","affiliation":[{"name":"Institute of Desert Meteorology, China Meteorological Administration, Urumqi 830002, China"},{"name":"National Observation and Research Station of Desert Meteorology, Taklimakan Desert of Xinjiang, Urumqi 830002, China"},{"name":"Taklimakan Desert Meteorology Field Experiment Station of China Meteorological Administration, Urumqi 830002, China"},{"name":"Xinjiang Key Laboratory of Desert Meteorology and Sandstorm, Urumqi 830002, China"},{"name":"Key Laboratory of Tree-Ring Physical and Chemical Research, China Meteorological Administration, Urumqi 830002, China"}],"role":[{"role":"author","vocabulary":"crossref"}]},{"ORCID":"https:\/\/orcid.org\/0000-0002-4188-5701","authenticated-orcid":false,"given":"Chenxiang","family":"Ju","sequence":"additional","affiliation":[{"name":"Institute of Desert Meteorology, China Meteorological Administration, Urumqi 830002, China"},{"name":"National Observation and Research Station of Desert Meteorology, Taklimakan Desert of Xinjiang, Urumqi 830002, China"},{"name":"Taklimakan Desert Meteorology Field Experiment Station of China Meteorological Administration, Urumqi 830002, China"},{"name":"Xinjiang Key Laboratory of Desert Meteorology and Sandstorm, Urumqi 830002, China"},{"name":"Key Laboratory of Tree-Ring Physical and Chemical Research, China Meteorological Administration, Urumqi 830002, China"}],"role":[{"role":"author","vocabulary":"crossref"}]},{"given":"Fan","family":"Yang","sequence":"additional","affiliation":[{"name":"Institute of Desert Meteorology, China Meteorological Administration, Urumqi 830002, China"},{"name":"National Observation and Research Station of Desert Meteorology, Taklimakan Desert of Xinjiang, Urumqi 830002, China"},{"name":"Taklimakan Desert Meteorology Field Experiment Station of China Meteorological Administration, Urumqi 830002, China"},{"name":"Xinjiang Key Laboratory of Desert Meteorology and Sandstorm, Urumqi 830002, China"},{"name":"Key Laboratory of Tree-Ring Physical and Chemical Research, China Meteorological Administration, Urumqi 830002, China"}],"role":[{"role":"author","vocabulary":"crossref"}]},{"ORCID":"https:\/\/orcid.org\/0000-0002-7861-2424","authenticated-orcid":false,"given":"Wen","family":"Huo","sequence":"additional","affiliation":[{"name":"Institute of Desert Meteorology, China Meteorological Administration, Urumqi 830002, China"},{"name":"National Observation and Research Station of Desert Meteorology, Taklimakan Desert of Xinjiang, Urumqi 830002, China"},{"name":"Taklimakan Desert Meteorology Field Experiment Station of China Meteorological Administration, Urumqi 830002, China"},{"name":"Xinjiang Key Laboratory of Desert Meteorology and Sandstorm, Urumqi 830002, China"},{"name":"Key Laboratory of Tree-Ring Physical and Chemical Research, China Meteorological Administration, Urumqi 830002, China"}],"role":[{"role":"author","vocabulary":"crossref"}]}],"member":"1968","published-online":{"date-parts":[[2023,12,14]]},"reference":[{"key":"ref_1","doi-asserted-by":"crossref","first-page":"D19106","DOI":"10.1029\/2010JD015192","article-title":"Changes of climate extremes in a typical arid zone: Observations and multimodel ensemble projections","volume":"116","author":"Yang","year":"2011","journal-title":"J. Geophys. Res."},{"key":"ref_2","doi-asserted-by":"crossref","first-page":"64060","DOI":"10.1088\/1748-9326\/ac0279","article-title":"Summer heat sources changes over the Tibetan Plateau in CMIP6 models","volume":"16","author":"Xie","year":"2021","journal-title":"Environ. Res. Lett."},{"key":"ref_3","doi-asserted-by":"crossref","first-page":"103957","DOI":"10.1016\/j.earscirev.2022.103957","article-title":"Recent climate and hydrological changes in a mountain\u2013basin system in Xinjiang, China","volume":"226","author":"Yao","year":"2022","journal-title":"Earth-Sci. Rev."},{"key":"ref_4","doi-asserted-by":"crossref","first-page":"6137237","DOI":"10.1155\/2020\/6137237","article-title":"Seasonal Variations of the Near-Surface Atmospheric Boundary Layer Structure in China\u2019s Gurbant\u00fcngg\u00fct Desert","volume":"2020","author":"Mamtimin","year":"2020","journal-title":"Adv. Meteorol."},{"key":"ref_5","first-page":"47","article-title":"Characteristics of surface radiation budget in Gurbantunggut Desert","volume":"41","author":"Gao","year":"2021","journal-title":"J. Desert Res."},{"key":"ref_6","first-page":"1","article-title":"Energy Budget Difference between Artificial Green Land and Natural Sandy Land in Taklimakan Desert","volume":"16","author":"Huo","year":"2022","journal-title":"Desert Oasis Meteorol."},{"key":"ref_7","first-page":"732","article-title":"Preliminary analysis of the relationship between vegetation change and surface heat source and precipitation in China over the Qinghai-Tibet Plateau","volume":"38","author":"Hua","year":"2008","journal-title":"Sci. China (Ser. D Earth Sci.)"},{"key":"ref_8","first-page":"755","article-title":"Impacts of the Tibetan Plateau winter\/spring snow depth and surface heat source on Asian summer monsoon: A review","volume":"42","author":"Duan","year":"2018","journal-title":"Chin. J. Atmos. Sci."},{"key":"ref_9","doi-asserted-by":"crossref","first-page":"124066","DOI":"10.1088\/1748-9326\/ab57a3","article-title":"Recent recovery of the boreal spring sensible heating over the Tibetan Plateau will continue in CMIP6 future projections","volume":"14","author":"Wang","year":"2019","journal-title":"Environ. Res. Lett."},{"key":"ref_10","doi-asserted-by":"crossref","first-page":"5671","DOI":"10.1175\/JCLI-D-11-00052.1","article-title":"Persistent Weakening Trend in the Spring Sensible Heat Source over the Tibetan Plateau and Its Impact on the Asian Summer Monsoon","volume":"24","author":"Duan","year":"2011","journal-title":"J. Clim."},{"key":"ref_11","first-page":"173","article-title":"Influence of sensible heat on planetary boundary layer height in East Asia","volume":"36","author":"Wan","year":"2017","journal-title":"Plateau Meteorol."},{"key":"ref_12","first-page":"1470","article-title":"The characteristics analysis on the summer atmospheric boundary layer height and surface heat fluxes over the Qinghai-Tibetan Plateau","volume":"37","author":"Su","year":"2018","journal-title":"Plateau Meteorol."},{"key":"ref_13","doi-asserted-by":"crossref","first-page":"7279","DOI":"10.1175\/JCLI-D-14-00859.1","article-title":"Characteristics of Heat Sources and Clouds over Eastern China and the Tibetan Plateau in Boreal Summer","volume":"28","author":"Chen","year":"2015","journal-title":"J. Clim."},{"key":"ref_14","doi-asserted-by":"crossref","first-page":"100","DOI":"10.1093\/nsr\/nwu045","article-title":"Tibetan Plateau climate dynamics: Recent research progress and outlook","volume":"2","author":"Wu","year":"2015","journal-title":"Natl. Sci. Rev."},{"key":"ref_15","doi-asserted-by":"crossref","first-page":"E1172","DOI":"10.1175\/BAMS-D-20-0236.1","article-title":"Desert Environment and Climate Observation Network over the Taklimakan Desert","volume":"102","author":"Yang","year":"2020","journal-title":"Bull. Am. Meteorol. Soc."},{"key":"ref_16","first-page":"983","article-title":"Surface heat source intensity and surface water\/energy balance in Shuanghu, northern Tibetan Plateau","volume":"69","author":"Guo","year":"2014","journal-title":"Acta Geogr. Sin."},{"key":"ref_17","first-page":"9","article-title":"Relationship between Surface Heating Fields over Qinghai-Xizang Plateau and Precipitation in Sichuan Basin during Summer","volume":"29","author":"Chen","year":"2003","journal-title":"Meteorological"},{"key":"ref_18","first-page":"979","article-title":"Advances in Studies of Pacific Decadal Oscillation","volume":"28","author":"Yang","year":"2004","journal-title":"Chin. J. Atmos. Sci."},{"key":"ref_19","doi-asserted-by":"crossref","first-page":"8810","DOI":"10.1029\/2004GL022015","article-title":"PDO, ENSO and the early summer monsoon rainfall over south China","volume":"32","author":"Chan","year":"2005","journal-title":"Geophys. Res. Lett."},{"key":"ref_20","doi-asserted-by":"crossref","first-page":"13008","DOI":"10.1002\/2013JD019862","article-title":"Modulation of PDO on the predictability of the interannual variability of early summer rainfall over south China","volume":"118","author":"Duan","year":"2013","journal-title":"J. Geophys. Res.-Atmos."},{"key":"ref_21","doi-asserted-by":"crossref","first-page":"950","DOI":"10.1175\/2010JHM1204.1","article-title":"Long-Term Temporal Variation of Extreme Rainfall Events in Australia: 1910\u20132006","volume":"11","author":"Fu","year":"2010","journal-title":"J. Hydrometeorol."},{"key":"ref_22","doi-asserted-by":"crossref","first-page":"468","DOI":"10.1002\/joc.4719","article-title":"Spatiotemporal variations of extreme precipitation regimes during 1961\u20132010 and possible teleconnections with climate indices across China","volume":"37","author":"Xiao","year":"2017","journal-title":"Int. J. Climatol."},{"key":"ref_23","doi-asserted-by":"crossref","first-page":"1607","DOI":"10.1007\/s00382-019-05078-4","article-title":"The strengthened relationship between the Yangtze River Valley summer rainfall and the Southern Hemisphere annular mode in recent decades","volume":"54","author":"Dou","year":"2020","journal-title":"Clim. Dynam."},{"key":"ref_24","doi-asserted-by":"crossref","first-page":"3369","DOI":"10.1007\/s00382-022-06511-x","article-title":"The global warming and IPO impacts on summer extreme precipitation in China","volume":"60","author":"Aihaiti","year":"2023","journal-title":"Clim. Dynam."},{"key":"ref_25","doi-asserted-by":"crossref","first-page":"1004","DOI":"10.1175\/1520-0442(1997)010<1004:ELIV>2.0.CO;2","article-title":"ENSO-like Interdecadal Variability: 1900\u201393","volume":"10","author":"Zhang","year":"1997","journal-title":"J. Clim."},{"key":"ref_26","doi-asserted-by":"crossref","first-page":"319","DOI":"10.1007\/s003820050284","article-title":"Inter-decadal modulation of the impact of ENSO on Australia","volume":"15","author":"Power","year":"1999","journal-title":"Clim. Dynam."},{"key":"ref_27","doi-asserted-by":"crossref","first-page":"2358","DOI":"10.1002\/2015GL063045","article-title":"Decadal changes in South Pacific sea surface temperatures and the relationship to the Pacific decadal oscillation and upper ocean heat content","volume":"42","author":"Linsley","year":"2015","journal-title":"Geophys. Res. Lett."},{"key":"ref_28","unstructured":"Mu\u00f1oz Sabater, J. (2023, January 08). ERA5-LAND Monthly Averaged Data from 1950 to Present. Copernicus Climate Change Service (C3S) Climate Data Store (CDS). Available online: https:\/\/cds.climate.copernicus.eu\/cdsapp#!\/dataset\/10.24381\/cds.68d2bb30?tab=overview."},{"key":"ref_29","doi-asserted-by":"crossref","first-page":"3077","DOI":"10.1007\/s00382-015-2525-1","article-title":"Tripole Index for the Interdecadal Pacific Oscillation","volume":"45","author":"Henley","year":"2015","journal-title":"Clim. Dynam."},{"key":"ref_30","doi-asserted-by":"crossref","first-page":"223","DOI":"10.1016\/S0168-1923(02)00109-0","article-title":"Energy balance closure at FLUXNET sites","volume":"113","author":"Wilson","year":"2002","journal-title":"Agr. Forest Meteorol."},{"key":"ref_31","first-page":"144","article-title":"Primary Study on Surface Heating Field and Biomass in Alpine Kobresia Meadow in the Qinghai-Tibetan Plateau","volume":"28","author":"Zhang","year":"2007","journal-title":"Chin. J. Agrometeorol."},{"key":"ref_32","doi-asserted-by":"crossref","first-page":"1999","DOI":"10.1002\/qj.3803","article-title":"The ERA5 global reanalysis","volume":"146","author":"Hersbach","year":"2020","journal-title":"Q. J. Roy. Meteor. Soc."},{"key":"ref_33","doi-asserted-by":"crossref","first-page":"683","DOI":"10.1111\/j.2517-6161.1991.tb01857.x","article-title":"A Reliable Data-Based Bandwidth Selection Method for Kernel Density Estimation","volume":"53","author":"Sheather","year":"1991","journal-title":"J. R. Stat. Society. Ser. B Methodol."},{"key":"ref_34","doi-asserted-by":"crossref","unstructured":"Coles, S. (2001). An Introduction to Statistical Modeling of Extreme Values, Springer.","DOI":"10.1007\/978-1-4471-3675-0"},{"key":"ref_35","unstructured":"Lane, D. (2003). Introduction to Statistics, Rice University."},{"key":"ref_36","unstructured":"Wei, F. (2007). The Current Statistical Climatic Diagnosis and Forecasting Technolog, Meteorological Press. (In Chinese)."},{"key":"ref_37","doi-asserted-by":"crossref","first-page":"1142","DOI":"10.1175\/2008JCLI2160.1","article-title":"A Statistical Downscaling Model for Southern Australia Winter Rainfall","volume":"22","author":"Li","year":"2009","journal-title":"J. Clim."},{"key":"ref_38","first-page":"1263","article-title":"Progress in the Study of Influence of the Qinghai-Xizang Plateau Land Atmosphere Interaction on East Asia Regional Climate","volume":"40","author":"Lai","year":"2021","journal-title":"Plateau Meteorol."},{"key":"ref_39","first-page":"543","article-title":"Climatological Characteristics of Ground Heat Sources over China","volume":"18","author":"Gao","year":"1995","journal-title":"J. Nanjing Inst. Meteorol."},{"key":"ref_40","doi-asserted-by":"crossref","first-page":"261","DOI":"10.1175\/JCLI-D-11-00669.1","article-title":"Trends in Summer Rainfall over China Associated with the Tibetan Plateau Sensible Heat Source during 1980\u20132008","volume":"26","author":"Duan","year":"2013","journal-title":"J. Clim."},{"key":"ref_41","unstructured":"Li, H. (2015). Land Surface Energy Exchange over Mainland China and Preliminary Analysis of Its Responses to Large-Scale Climate Change. [Ph.D. Thesis, Nanjing University]. (In Chinese)."},{"key":"ref_42","unstructured":"Du, Y. (2018). The Interaction between Land Surface and Atmosphe Ric Boundary Layer in Northwest Region and Its Response to the Summer Monsoon. [Master\u2019s Thesis, Lanzhou University]. (In Chinese)."},{"key":"ref_43","doi-asserted-by":"crossref","unstructured":"Aguedjou, H.M.A., Chaigneau, A., Dadou, I., Morel, Y., Balo\u00eftcha, E., and Da-Allada, C.Y. (2023). Imprint of Mesoscale Eddies on Air-Sea Interaction in the Tropical Atlantic Ocean. Remote Sens., 15.","DOI":"10.3390\/rs15123087"}],"container-title":["Remote Sensing"],"original-title":[],"language":"en","link":[{"URL":"https:\/\/www.mdpi.com\/2072-4292\/15\/24\/5731\/pdf","content-type":"unspecified","content-version":"vor","intended-application":"similarity-checking"}],"deposited":{"date-parts":[[2025,10,10]],"date-time":"2025-10-10T21:39:01Z","timestamp":1760132341000},"score":1,"resource":{"primary":{"URL":"https:\/\/www.mdpi.com\/2072-4292\/15\/24\/5731"}},"subtitle":[],"short-title":[],"issued":{"date-parts":[[2023,12,14]]},"references-count":43,"journal-issue":{"issue":"24","published-online":{"date-parts":[[2023,12]]}},"alternative-id":["rs15245731"],"URL":"https:\/\/doi.org\/10.3390\/rs15245731","relation":{},"ISSN":["2072-4292"],"issn-type":[{"type":"electronic","value":"2072-4292"}],"subject":[],"published":{"date-parts":[[2023,12,14]]}}}