P. A. Inchin, C. Heale, M. D. Zettergren, B. Bergsson, S. Debchoudhury, S. Chakraborty
{"title":"恶劣天气产生的声波和重力波对电离层的影响:一个模式引导的案例研究","authors":"P. A. Inchin, C. Heale, M. D. Zettergren, B. Bergsson, S. Debchoudhury, S. Chakraborty","doi":"10.1029/2025JA034012","DOIUrl":null,"url":null,"abstract":"<p>Acoustic and gravity waves (AGWs) generated by tropospheric weather are known sources of fluctuations in the ionosphere—traveling ionospheric disturbances (TIDs). Despite their importance, the effects of AGWs on the ionosphere, including associated energy and momentum deposition, remain poorly quantified. To address this gap, we present our first three-dimensional numerical simulations of coupled atmosphere-ionosphere dynamics during a typical severe terrestrial weather episode over the continental United States in May 2017. Using the nonlinear compressible models MAGIC and GEMINI, we reproduced many of the salient features of AGW-driven TIDs in slant total electron content. Simulation results reveal that although AGW-TID amplitudes reach only <span></span><math>\n <semantics>\n <mrow>\n <mo>∼</mo>\n </mrow>\n <annotation> ${\\sim} $</annotation>\n </semantics></math>0.35 TECu (<span></span><math>\n <semantics>\n <mrow>\n <mo>∼</mo>\n </mrow>\n <annotation> ${\\sim} $</annotation>\n </semantics></math>2–3<span></span><math>\n <semantics>\n <mrow>\n <mi>%</mi>\n </mrow>\n <annotation> $\\%$</annotation>\n </semantics></math> of absolute vTEC), AGWs induce substantial ionospheric fluctuations, up to 70 K in ion and 120 K in electron temperatures (<span></span><math>\n <semantics>\n <mrow>\n <mo>∼</mo>\n </mrow>\n <annotation> ${\\sim} $</annotation>\n </semantics></math>10–16<span></span><math>\n <semantics>\n <mrow>\n <mi>%</mi>\n </mrow>\n <annotation> $\\%$</annotation>\n </semantics></math> of ambient state), as well as <span></span><math>\n <semantics>\n <mrow>\n <mo>∼</mo>\n <mn>10</mn>\n <mi>%</mi>\n </mrow>\n <annotation> ${\\sim} 10\\%$</annotation>\n </semantics></math> in electron density at 100–300 km altitudes. Furthermore, long-period AGW impacts (lasting several hours), continuously generated by the evolving weather system, result in significant redistribution of plasma and modification of electron density ambient state by more than <span></span><math>\n <semantics>\n <mrow>\n <mo>∼</mo>\n <mn>20</mn>\n <mi>%</mi>\n </mrow>\n <annotation> ${\\sim} 20\\%$</annotation>\n </semantics></math> in the E and bottom F regions of the ionosphere. These modifications can plausibly affect various communication and navigation system applications, highlighting the need to incorporate AGW effects into space weather forecasts.</p>","PeriodicalId":15894,"journal":{"name":"Journal of Geophysical Research: Space Physics","volume":"130 10","pages":""},"PeriodicalIF":2.9000,"publicationDate":"2025-09-26","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Severe Weather-Generated Acoustic and Gravity Wave Impacts on the Ionosphere: A Model-Guided Case Study\",\"authors\":\"P. A. Inchin, C. Heale, M. D. Zettergren, B. Bergsson, S. Debchoudhury, S. Chakraborty\",\"doi\":\"10.1029/2025JA034012\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<p>Acoustic and gravity waves (AGWs) generated by tropospheric weather are known sources of fluctuations in the ionosphere—traveling ionospheric disturbances (TIDs). Despite their importance, the effects of AGWs on the ionosphere, including associated energy and momentum deposition, remain poorly quantified. To address this gap, we present our first three-dimensional numerical simulations of coupled atmosphere-ionosphere dynamics during a typical severe terrestrial weather episode over the continental United States in May 2017. Using the nonlinear compressible models MAGIC and GEMINI, we reproduced many of the salient features of AGW-driven TIDs in slant total electron content. Simulation results reveal that although AGW-TID amplitudes reach only <span></span><math>\\n <semantics>\\n <mrow>\\n <mo>∼</mo>\\n </mrow>\\n <annotation> ${\\\\sim} $</annotation>\\n </semantics></math>0.35 TECu (<span></span><math>\\n <semantics>\\n <mrow>\\n <mo>∼</mo>\\n </mrow>\\n <annotation> ${\\\\sim} $</annotation>\\n </semantics></math>2–3<span></span><math>\\n <semantics>\\n <mrow>\\n <mi>%</mi>\\n </mrow>\\n <annotation> $\\\\%$</annotation>\\n </semantics></math> of absolute vTEC), AGWs induce substantial ionospheric fluctuations, up to 70 K in ion and 120 K in electron temperatures (<span></span><math>\\n <semantics>\\n <mrow>\\n <mo>∼</mo>\\n </mrow>\\n <annotation> ${\\\\sim} $</annotation>\\n </semantics></math>10–16<span></span><math>\\n <semantics>\\n <mrow>\\n <mi>%</mi>\\n </mrow>\\n <annotation> $\\\\%$</annotation>\\n </semantics></math> of ambient state), as well as <span></span><math>\\n <semantics>\\n <mrow>\\n <mo>∼</mo>\\n <mn>10</mn>\\n <mi>%</mi>\\n </mrow>\\n <annotation> ${\\\\sim} 10\\\\%$</annotation>\\n </semantics></math> in electron density at 100–300 km altitudes. Furthermore, long-period AGW impacts (lasting several hours), continuously generated by the evolving weather system, result in significant redistribution of plasma and modification of electron density ambient state by more than <span></span><math>\\n <semantics>\\n <mrow>\\n <mo>∼</mo>\\n <mn>20</mn>\\n <mi>%</mi>\\n </mrow>\\n <annotation> ${\\\\sim} 20\\\\%$</annotation>\\n </semantics></math> in the E and bottom F regions of the ionosphere. These modifications can plausibly affect various communication and navigation system applications, highlighting the need to incorporate AGW effects into space weather forecasts.</p>\",\"PeriodicalId\":15894,\"journal\":{\"name\":\"Journal of Geophysical Research: Space Physics\",\"volume\":\"130 10\",\"pages\":\"\"},\"PeriodicalIF\":2.9000,\"publicationDate\":\"2025-09-26\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Journal of Geophysical Research: Space Physics\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2025JA034012\",\"RegionNum\":2,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q2\",\"JCRName\":\"ASTRONOMY & ASTROPHYSICS\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of Geophysical Research: Space Physics","FirstCategoryId":"89","ListUrlMain":"https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2025JA034012","RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"ASTRONOMY & ASTROPHYSICS","Score":null,"Total":0}
Severe Weather-Generated Acoustic and Gravity Wave Impacts on the Ionosphere: A Model-Guided Case Study
Acoustic and gravity waves (AGWs) generated by tropospheric weather are known sources of fluctuations in the ionosphere—traveling ionospheric disturbances (TIDs). Despite their importance, the effects of AGWs on the ionosphere, including associated energy and momentum deposition, remain poorly quantified. To address this gap, we present our first three-dimensional numerical simulations of coupled atmosphere-ionosphere dynamics during a typical severe terrestrial weather episode over the continental United States in May 2017. Using the nonlinear compressible models MAGIC and GEMINI, we reproduced many of the salient features of AGW-driven TIDs in slant total electron content. Simulation results reveal that although AGW-TID amplitudes reach only 0.35 TECu (2–3 of absolute vTEC), AGWs induce substantial ionospheric fluctuations, up to 70 K in ion and 120 K in electron temperatures (10–16 of ambient state), as well as in electron density at 100–300 km altitudes. Furthermore, long-period AGW impacts (lasting several hours), continuously generated by the evolving weather system, result in significant redistribution of plasma and modification of electron density ambient state by more than in the E and bottom F regions of the ionosphere. These modifications can plausibly affect various communication and navigation system applications, highlighting the need to incorporate AGW effects into space weather forecasts.