Jyotirmoy Kalita, Manoj K. Mishra, Prakash Chauhan, Anirban Guha
{"title":"火星终结者上的云层:通过火星彩色照相机 (MCC) 在 MY32 至 34 期间拍摄的图像进行的研究","authors":"Jyotirmoy Kalita, Manoj K. Mishra, Prakash Chauhan, Anirban Guha","doi":"10.1007/s12524-024-01866-6","DOIUrl":null,"url":null,"abstract":"<p>The present study reports a cloud feature observed by the Mars Colour Camera (MCC) onboard India’s first Mars Orbiter Mission in both the Martian terminator during the MY 32 to 34: “The Twilight Cloud”. Twilight clouds used to show latitudinal expansion, covering over 5,000 km<sup>2</sup> and used to appear between 19:00 LT and 20:00 LT for evening and 04:00 LT and 05:00 LT for morning terminator. These clouds often reached altitudes of at least 15 to 40 km. We further compare these observations to Mars Climate Sounder (MCS) data. The TOA (Top of the Atmosphere) reflectance varies from 0.030 to 0.035 in the blue channel and 0.025 to 0.030 in the red channel indicates the presence of both dust and water ice at the observed altitude level. The MCD-GCM (Mars Climate Database Web Interface- General Circulation Model) simulations used to estimate the mixing ratio. MCS extinction data along with simulated MCD results, estimated the effective radius of the particle to be varying from 0.3 to 3.0 μm. The work also infers the seasonal behaviour of these clouds, especially during NHS (Northern Hemisphere Summer) and LNHA (Late Northern Hemisphere Autumn). The present work indicates that the daily thermal variation is one of the plausible reasons for the formation of the clouds.</p>","PeriodicalId":17510,"journal":{"name":"Journal of the Indian Society of Remote Sensing","volume":"1 1","pages":""},"PeriodicalIF":2.2000,"publicationDate":"2024-05-28","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Clouds on Martian Terminator: A Study Through the Images Captured by the Mars Colour Camera (MCC) During MY32 to 34\",\"authors\":\"Jyotirmoy Kalita, Manoj K. Mishra, Prakash Chauhan, Anirban Guha\",\"doi\":\"10.1007/s12524-024-01866-6\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<p>The present study reports a cloud feature observed by the Mars Colour Camera (MCC) onboard India’s first Mars Orbiter Mission in both the Martian terminator during the MY 32 to 34: “The Twilight Cloud”. Twilight clouds used to show latitudinal expansion, covering over 5,000 km<sup>2</sup> and used to appear between 19:00 LT and 20:00 LT for evening and 04:00 LT and 05:00 LT for morning terminator. These clouds often reached altitudes of at least 15 to 40 km. We further compare these observations to Mars Climate Sounder (MCS) data. The TOA (Top of the Atmosphere) reflectance varies from 0.030 to 0.035 in the blue channel and 0.025 to 0.030 in the red channel indicates the presence of both dust and water ice at the observed altitude level. The MCD-GCM (Mars Climate Database Web Interface- General Circulation Model) simulations used to estimate the mixing ratio. MCS extinction data along with simulated MCD results, estimated the effective radius of the particle to be varying from 0.3 to 3.0 μm. The work also infers the seasonal behaviour of these clouds, especially during NHS (Northern Hemisphere Summer) and LNHA (Late Northern Hemisphere Autumn). The present work indicates that the daily thermal variation is one of the plausible reasons for the formation of the clouds.</p>\",\"PeriodicalId\":17510,\"journal\":{\"name\":\"Journal of the Indian Society of Remote Sensing\",\"volume\":\"1 1\",\"pages\":\"\"},\"PeriodicalIF\":2.2000,\"publicationDate\":\"2024-05-28\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Journal of the Indian Society of Remote Sensing\",\"FirstCategoryId\":\"5\",\"ListUrlMain\":\"https://doi.org/10.1007/s12524-024-01866-6\",\"RegionNum\":4,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q3\",\"JCRName\":\"ENVIRONMENTAL SCIENCES\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of the Indian Society of Remote Sensing","FirstCategoryId":"5","ListUrlMain":"https://doi.org/10.1007/s12524-024-01866-6","RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q3","JCRName":"ENVIRONMENTAL SCIENCES","Score":null,"Total":0}
Clouds on Martian Terminator: A Study Through the Images Captured by the Mars Colour Camera (MCC) During MY32 to 34
The present study reports a cloud feature observed by the Mars Colour Camera (MCC) onboard India’s first Mars Orbiter Mission in both the Martian terminator during the MY 32 to 34: “The Twilight Cloud”. Twilight clouds used to show latitudinal expansion, covering over 5,000 km2 and used to appear between 19:00 LT and 20:00 LT for evening and 04:00 LT and 05:00 LT for morning terminator. These clouds often reached altitudes of at least 15 to 40 km. We further compare these observations to Mars Climate Sounder (MCS) data. The TOA (Top of the Atmosphere) reflectance varies from 0.030 to 0.035 in the blue channel and 0.025 to 0.030 in the red channel indicates the presence of both dust and water ice at the observed altitude level. The MCD-GCM (Mars Climate Database Web Interface- General Circulation Model) simulations used to estimate the mixing ratio. MCS extinction data along with simulated MCD results, estimated the effective radius of the particle to be varying from 0.3 to 3.0 μm. The work also infers the seasonal behaviour of these clouds, especially during NHS (Northern Hemisphere Summer) and LNHA (Late Northern Hemisphere Autumn). The present work indicates that the daily thermal variation is one of the plausible reasons for the formation of the clouds.
期刊介绍:
The aims and scope of the Journal of the Indian Society of Remote Sensing are to help towards advancement, dissemination and application of the knowledge of Remote Sensing technology, which is deemed to include photo interpretation, photogrammetry, aerial photography, image processing, and other related technologies in the field of survey, planning and management of natural resources and other areas of application where the technology is considered to be appropriate, to promote interaction among all persons, bodies, institutions (private and/or state-owned) and industries interested in achieving advancement, dissemination and application of the technology, to encourage and undertake research in remote sensing and related technologies and to undertake and execute all acts which shall promote all or any of the aims and objectives of the Indian Society of Remote Sensing.