Article(id=1242137486193926378, tenantId=1146029695717560320, journalId=1146031591421210625, issueId=1242137460445098003, articleNumber=null, orderNo=16, doi=10.3981/j.issn.1000-7857.2019.06.014, pmid=null, cstr=null, oa=null, hot=null, price=null, onlineType=0, articleFormat=0, articleType=null, articleTypeStr=null, receivedDate=1541001600000, receivedDateStr=2018-11-01, revisedDate=1544889600000, revisedDateStr=2018-12-16, acceptedDate=null, acceptedDateStr=null, onlineDate=1554799288813, onlineDateStr=2019-04-09, pubDate=1553702400000, pubDateStr=2019-03-28, doiRegisterDate=null, doiRegisterDateStr=null, onlineIssueDate=1554799288813, onlineIssueDateStr=2019-04-09, onlineJustAcceptDate=null, onlineJustAcceptDateStr=null, onlineFirstDate=null, onlineFirstDateStr=null, sourceXml=null, magXml=null, createTime=1774078254503, creator=sys-migrate, updateTime=1774078254503, updator=sys-migrate, issue=Issue{id=1242137460445098003, tenantId=1146029695717560320, journalId=1146031591421210625, year='2019', volume='37', issue='6', pageStart='1', pageEnd='128', issueExtLink='null', onlineDate='null', pubDate='1553702400000', pubDateStr='2019-03-28', beforeIssueId=null, nextIssueId=null, price=null, status=1, issueComplete=1, articleOrder=3, issueType=-1, specialIssue=null, createTime=1774078248364, creator='sys-migrate', updateTime=1774078248364, updator='sys-migrate', preIssue=null, nextIssue=null, articleTotal=null, ext=null, issueFiles=null, downloadFileDto=null}, startPage=104, endPage=113, ext={EN=ArticleExt(id=1242137491982065919, articleId=1242137486193926378, tenantId=1146029695717560320, journalId=1146031591421210625, language=EN, title=Variations of thermospheric density during equinox and solstice, columnId=1242116080374710456, journalTitle=Science & Technology Review, columnName=Articles, runingTitle=null, highlight=null, articleAbstract=The thermospheric neutral density sees a strong variation during equinoxes and solstices due to the solar insolation variation. The long-term continual data from Chinese Atmospheric Density Detector installed on the satellite are used to study this variation, The main results of this study are that the thermospheric density has an obvious symmetry around March equinox and September equinox; the thermosphere density has an obvious asymmetry around June solstice and December solstice; the variations have an obvious hemispheric asymmetry in high latitude (around 80 degrees); the proportion of the atmospheric density is 3~3.6 times at the height of 670 km, 13 times at the height of 560 km; the latitude and the altitude contribute to this asymmetry; the comparison of the measured data and the NRLMSISE00 data shows that the NRLMSISE00 data cannot fully respond to the summer and winter hemisphere atmospheric density variations., authors=LI Yongping1,2,3 , SUN Yueqiang1,2,3 , WANG Xinyue1,2,3 , FU Zhenyu1,2,3 , authorsList=LI Yongping, SUN Yueqiang, WANG Xinyue, FU Zhenyu, authorCompany=1. National Space Science Center, Chinese Academy of Sciences, Beijing Key Laboratory of Space Environment Exploration, Beijing 100190, China;1,2,3 , 孙越强1,2,3 , 王馨悦1,2,3 , 付振宇1,2,3 , authorsList=李永平, 孙越强, 王馨悦, 付振宇, authorCompany=1. 中国科学院国家空间科学中心, 天基空间环境探测北京市重点实验室, 北京 100190;
科技导报
| 研究论文 2019, 37(6): 104-113
两分两至点热层大气密度变化
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李永平1,2,3 , 孙越强1,2,3 , 王馨悦1,2,3 , 付振宇1,2,3
作者信息
1. 中国科学院国家空间科学中心, 天基空间环境探测北京市重点实验室, 北京 100190;
Variations of thermospheric density during equinox and solstice
Affiliations
出版时间: 2019-03-28
doi: 10.3981/j.issn.1000-7857.2019.06.014
文章导航
热层大气受太阳辐射的影响，其变化与光照时间长短密切相关，在春分、秋分、夏至、冬至期间呈现出不同的特点。通过在中国低轨道航天器上装载大气密度探测器，获得在轨原位探测数据，分析大气密度在两分两至点时的变化关系。结果表明，春分和秋分（两分点）期间全球热层大气密度随纬度对称性变化，但夏至和冬至（两至点）期间则呈现出全球热层大气密度的南北半球不对称性变化；两至点期间南北半球分别处于夏半球和冬半球，在南北高纬地区（纬度80°附近）670 km上空热层大气密度存在显著差异，探测值表示出3~3.6倍的差异，而在560 km高度上探测到两者差异可高达13倍左右，不对称程度与高度和纬度有关；探测值与模式值比较表明，模式值对冬夏半球上空热层大气密度差异变化显著响应不足。
两至点(夏至、冬至)
/
热层大气密度
/
太阳远紫外辐射
The thermospheric neutral density sees a strong variation during equinoxes and solstices due to the solar insolation variation. The long-term continual data from Chinese Atmospheric Density Detector installed on the satellite are used to study this variation, The main results of this study are that the thermospheric density has an obvious symmetry around March equinox and September equinox; the thermosphere density has an obvious asymmetry around June solstice and December solstice; the variations have an obvious hemispheric asymmetry in high latitude (around 80 degrees); the proportion of the atmospheric density is 3~3.6 times at the height of 670 km, 13 times at the height of 560 km; the latitude and the altitude contribute to this asymmetry; the comparison of the measured data and the NRLMSISE00 data shows that the NRLMSISE00 data cannot fully respond to the summer and winter hemisphere atmospheric density variations.
Jure solstic and Devember solstice
/
atmospheric density
/
solar far ultraviolet radiation
李永平, 孙越强, 王馨悦, 付振宇.
两分两至点热层大气密度变化.
科技导报,
2019
, 37
(6)
: 104
-113
.
DOI: 10.3981/j.issn.1000-7857.2019.06.014
LI Yongping, SUN Yueqiang, WANG Xinyue, FU Zhenyu.
Variations of thermospheric density during equinox and solstice[J].
Science & Technology Review ,
2019
, 37
(6)
: 104
-113
.
DOI: 10.3981/j.issn.1000-7857.2019.06.014
2019年第37卷第6期
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文章信息
doi: 10.3981/j.issn.1000-7857.2019.06.014
接收时间：2018-11-01
首发时间：2019-04-09
出版时间：2019-03-28
收稿日期：2018-11-01
修回日期：2018-12-16
https://castjournals.cast.org.cn/joweb/kjdb/CN/10.3981/j.issn.1000-7857.2019.06.014
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2种不同金属材料的力学参数
科 属数 种数 占总种数比例 属 种数 占总种数比例 鹅膏菌科Amanitaceae 2 11 5.26 鹅膏菌属 Amanita 10 4.78 小菇科 Mycenaceae 2 12 5.74 丝盖伞属 Inocybe 5 2.39 多孔菌科 Polyporaceae 8 14 6.70 蜡蘑属 Laccaria 5 2.39 红菇科 Russulaceae 3 23 11.00 小皮伞属 Marasmius 6 2.87 小菇属 Mycena 11 5.26 光柄菇属 Pluteus 5 2.39 红菇属 Russula 17 8.13 栓菌属 Trametes 5 2.39
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