{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2025,10,12]],"date-time":"2025-10-12T04:41:15Z","timestamp":1760244075483,"version":"build-2065373602"},"reference-count":34,"publisher":"MDPI AG","issue":"4","license":[{"start":{"date-parts":[[2008,10,13]],"date-time":"2008-10-13T00:00:00Z","timestamp":1223856000000},"content-version":"vor","delay-in-days":0,"URL":"https:\/\/creativecommons.org\/licenses\/by\/3.0\/"}],"content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":["Entropy"],"abstract":"<jats:p>The universal principle that an open system can be driven to a state far from equilibrium, or organized, by strong negative entropy flow from its surroundings has been validated in numerous fields from physics and chemistry to the life science. In this paper, entropy flows for a severe storm are calculated via the entropy flow formula using the National Centers for Environmental Prediction\/National Center for Atmospheric Research reanalysis data. The results show that the intensification of negative (positive) entropy flow entering into the storm preceded the strengthening (weakening) of its intensity, implying that entropy flow analysis can be used as a potential tool in forecasting changes in the intensity of a storm.<\/jats:p>","DOI":"10.3390\/e10040430","type":"journal-article","created":{"date-parts":[[2008,10,14]],"date-time":"2008-10-14T02:50:42Z","timestamp":1223952642000},"page":"430-440","update-policy":"https:\/\/doi.org\/10.3390\/mdpi_crossmark_policy","source":"Crossref","is-referenced-by-count":1,"title":["Entropy Flow and the Evolution of a Storm"],"prefix":"10.3390","volume":"10","author":[{"given":"Ying","family":"Liu","sequence":"first","affiliation":[{"name":"State Key Laboratory of Severe Weather, Chinese Academy of Meteorological Sciences, Beijing 100081, P. R. China"}]},{"given":"Chongjian","family":"Liu","sequence":"additional","affiliation":[{"name":"State Key Laboratory of Severe Weather, Chinese Academy of Meteorological Sciences, Beijing 100081, P. R. China"}]}],"member":"1968","published-online":{"date-parts":[[2008,10,13]]},"reference":[{"key":"ref_1","doi-asserted-by":"crossref","first-page":"441","DOI":"10.1175\/1520-0442(1997)010<0441:TOAGMS>2.0.CO;2","article-title":"Thermodynamics of a Global-Mean State of the Atmosphere-A State of Maximum Entropy Increase","volume":"10","author":"Ozawa","year":"1997","journal-title":"J. Climate"},{"key":"ref_2","first-page":"605","article-title":"Entropy of a connecting water-air system and the interpretation of cloud morphogenesis","volume":"123","author":"Duane","year":"1997","journal-title":"Q. J. R. Meteorol. 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