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利用F10.7和Mg II构建太阳极紫外辐射长时间序列   总被引:3,自引:1,他引:2       下载免费PDF全文
利用SOHO/SEM在1996-2008年的太阳EUV观测数据,比较和评估F10.7和Mg II作为EUV代理参数的代表性,不能支持Viereck等关于Mg II是比F10.7更好的代理参数的结论.通过比较对两种参数的多种回归计算结果,确立双因子极大似然估计方法构建EUV计算模式,通过模型计算结果与SEM观测数据比较,表明该模型能够很好地重建EUV数据系列.利用该模式,构建了1978年11月以来的太阳极紫外辐射数据序列.  相似文献   
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The paper presents the seasonal variation of 6300 Å line intensity at Calcutta with relative sunspot number, solar flare number and variable component of 10.7 cm solar flux. A study has been made and important results have been obtained which are as follows. (i) Intensity of 6300 Å line shows periodic variation with relative sunspot number, solar flare number and variable component of 10.7 cm solar flux during the period 1984–1986 which is the secondary peak of the descending phase of 21st solar cycle. (ii) 6300 Å line intensity at Cachoeira Paulista station, taken by Sahai et al. (1988), also shows periodic variation with solar parameters during the period 1978–1980 which is the peak phase of the solar cycle. (iii) A possible explanation of such a type of variation is also presented.  相似文献   
3.
本文利用南极中山站(ZHS),以及北极与其地理共轭的Tromso站(TRO)、地磁共轭的Longyearbyen站(LYB)各自约一个太阳活动周的观测数据,对比分析了极区电离层F2层峰值电子浓度(NmF2)对太阳活动的依赖性.结果表明,三个台站NmF2月中值随修正太阳10.7 cm通量指数F10.7P(简称P)增大在总体上呈线性增长,这说明在这三个台站,太阳辐射仍是其F2层主要电离源.其中TRO站NmF2与P线性关系最好,ZHS站的次之,LYB站的最差.在日变化中,TRO站NmF2对太阳活动响应最为敏感的时刻出现在地方时中午附近,LYB站出现在磁中午,ZHS站则出现在地方时中午和磁地方时中午之间.这主要是由地理/地磁纬度差异引起的不同强度的光致电离与极区等离子体对流共同作用的结果.在年变化中,TRO站NmF2随太阳活动变化上升最快的季节出现在冬季,夏季上升最慢.在ZHS站与LYB站,NmF2对太阳活动变化的响应都在两分季最为敏感.这种季节上的差异则是由于三个台站光致电离与中性大气成分R[O/N2]的不同所致.  相似文献   
4.
利用中山站1995-2006年的电离层垂测数据统计分析了当地电离层F2层峰值电子浓度(NmF2)对太阳活动变化的依赖性,研究发现在中山站NmF2月中值随修正太阳10.7厘米通量指数F10.7P增大而增大,其饱和或放大趋势不明显。除冬季12-16 UT、20-2 UT与夏季2-11 UT以外的绝大部分时刻,两者具有良好的线性关系。NmF2月中值随F10.7P变化斜率随季节、地方时而变化。在日变化中,NmF2随F10.7P变化斜率极大值出现在磁中午附近,明显大于其他时刻,在夜侧变化斜率整体较小,且在分季和冬季的夜侧以及夏季全天,其斜率随地方时变化不大。在年变化中,日侧斜率最大值出现在两分季,冬季次之,夏季最小;而夜侧斜率在夏半年(10月-3月)整体上要大于冬半年(4月-9月)。结合中山站位于极隙区纬度的特殊地理位置,分析了上述NmF2变化特征的可能原因。  相似文献   
5.
The paper presents the variation of 5577 Å line intensity with relative sunspot number, and 10.7 cm solar flux. The study has obtained the following important results.[(i)] The 5577 Å line intensity at Calcutta is plotted against relative sunspot number, and the variable component of 10.7 cm solar flux during 1984–1985, which is the secondary peak of the descending phase of the 21st solar cycle. The intensity curves show periodic variation with different solar parameters.[(ii)] The 5577 Å line intensity at Mt. Abu also shows periodic variation with solar parameters during the period 1965–1968 when there was a peak phase of the 20th solar cycle.[(iii)] A possible explanation for such variation is also presented.  相似文献   
6.
Ionospheric electron content (IEC) and slab thickness () data for the period 1977 to 1980 from Lunping (23.03°N; 121.90°E subionospheric) have been examined for their solar activity dependence. Local noontime monthly means as well as values for the 5 QQ days in a month have been examined separately with different solar indices, namely: solar EUV flux (170–190 Å),S 10.7 cm flux and sun spot number (SSN) on a seasonal basis. Both IEC and parameters exhibit better correlation with solar EUV andS 10.7 cm fluxes than with SSN for all seasons. IEC increases linearly with both EUV andS 10.7 cm flux whereas with SSN it shows a distinct nonlinear relationship during all seasons in both monthly mean and 5 QQ days' values. This study indicates that for correlating and predicting the variations (especially the medium term) in the ionospheric parameters, both EUV andS 10.7 cm fluxes have an advantage over SSN.  相似文献   
7.
由于全球卫星导航系统(GNSS)技术广泛应用,各个领域行业对GNSS数据处理的精度和效率提出了更高要求,本文基于GAMIT/GLOBK 10.7与Bernese 5.2软件对中国大陆构造环境监测网络(CMONOC)观测数据进行解算,并对解算策略的确定和解算结果进行对比分析,实验结果表明:GAMIT 10.7和Berne...  相似文献   
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