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1.
以新月时月亮的射电辐射为温度基准和准口面温度定标的方法，在２２ＧＨｚ频率上于１９９３年７月～３月测量了１３．７ｍ射电望远镜抛物面天线的增益。根据测量的增益值（６７．１０─±０．０７ｄｂ）定标了太阳射电流量，流量测量的系统差为±５．８％，偶然差为±２．７％，测量的宁静太阳亮温度（非源区）为１０１００±３００Ｋ。除此之外，还推导和计算了不同源模型下的天线方向图改正因子Ｋｓ，并计算了太阳射电源的流量密度。 相似文献
2.
在１９９５ 年至１９９７ 年,用２ ．１６ 米望远镜,５０?／ｍ ｍ 色散观测了仙后座１９９５ 新星的光谱．１９９５ 年的光谱以Ｆｅ Ⅱ及Ｈ Ⅰ的发射线为主要特征,所有发射线呈ＰＣｙｇ 轮廓,１９９６ 年光谱主要是Ｈ Ⅰ及Ｈｅ Ⅰ的发射,１９９７ 年光谱呈现很强的［Ｆｅ Ｘ］ 、［Ｆｅ ＶⅡ］ 、［Ｏ Ⅲ］ 发射,表明新星已进入星云阶段．以观测谱的连续谱估算了抛射物质的有效温度,算得１９９５ 年１０ 月１４ 日温度为２１３００Ｋ、１９９６ 年１０ 月２６ 日为９７００Ｋ、１９９７ 年１２ 月１６ 日为１０２００Ｋ．以测量谱线的流量估算抛射物质总质量约４ ．７ ×１０ － ５ Ｍ⊙,氦的丰度为ＮＨｅ／ＮＨ＝ ０ ．０４７ ． 相似文献
3.
以新月时月亮的射电辐射为温度基准和准口面温度定标的方法，在２２ＧＨｚ频率上于１９９３年７月￣８月测量了１３．７ｍ射电望远镜抛物面天线的增益，根据测量的增益值（６７．１０±０．０７ｄｂ）定标了太阳射电流量。流量测量的系统差为±５．８％，偶然差为±２．７％，测量的宁静太阳亮温度（非源区）为１０１００±３００Ｋ。除此之外，还推导和计算了不同源模型下的天线方向图改正因子Ｋｓ，并计算了太阳射电源的流量密度。 相似文献
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5.
孙九祯 《紫金山天文台台刊》1995,14(2):95-103
本文根据１９８７年９月２３日的８．６毫米波段射电日食观测资料，计算了太阳射电的径向亮温度分布，计算结果表明：８．６毫米波段太阳径向亮温度分布呈临边增亮；增亮幅度相对于日面中心部分为５．１％，中国部分也存在着增亮的征兆；日食当天８．６毫米波段太阳射电辐射的剖流量为２３４６Ｓ、ｆ、Ｕ；食甚时的剩余流量约为１２．５％，掩食半径为１．０１４光学太阳半径。 相似文献
6.
IRI-86(国际参考电离层-86)是COSPAR和国际无线电科学联合会(URSI)推荐的全球电离层标准模式的1986年版。IRI的这个版本,通过运行它的程序可以给出确定地点(地理坐标或地磁坐标)、时刻(地方时或世界时)、季节(年日或月日)、太阳活动(平均太阳黑子数或10.7CM太阳辐射通量)的电子密度、电子温度,离子温度和O~ 、H~ 、He~ 、No~ 以及O_2~ 浓度的廓线。 IRI-86代表全球电离层各个月的平均状态,其作者明确指出了它的如下局限: 1、IRI-86提供的是平均值,与具体时刻测量值的偏差可达25％。 2、不包括极光纬度区域的电离层状况。 3、不包括电离层不均匀结构(即不包括Sprad F和磁暴发生时的情况)。 4、其依据的是1950年—1975年的实测资料,因此,IRI-86对太阳活数指数有限制,要求太阳黑子数(12个月的滑动平均值)小于130。 本文将IRI-86的计算值与我国电离层实测值进行对比。实测值取自1965—1976年满洲里、乌鲁木齐、海南岛、重庆等四个测站的月报表。比较的结果为: 1、F_oF1和F_oE的模式值和测量值不论是太阳活动高年还是太阳活动低年、不论夏季或冬季都符合得比较好。F_oF2的模式值与实测值有比较明显的偏差。 2、除去中纬台站(满州里、乌鲁木齐)在午夜后日出前的一些时刻,F_oF2月中值的偏差超过25％外,其它时间 相似文献
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１９９７年３月９日日全食８．６ｍｍ波段射电观测资料的分析表明,８．６ｍｍ波段射电太阳的半径为１．０１２Ｒ,总流量为２５４０ｓｆｕ（１ｓｆｕ＝１０＾－２２Ｗ／ｍ＾２Ｈｚ）,日面平均亮温度为９６３２Ｋ,径向亮温度分布,在日面光学边缘内侧０．９３６－０．９９２Ｒ处,存在临边增亮,平均增亮幅度相对于日面中心为９．７％。 相似文献
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１９９７年３月９日日全食８．６ｍｍ波段射电观测资料的分析表明：８．６ｍｍ波段射电太阳的半径为１．０１２Ｒ,总流量为２５４０ｓｆｕ（１ｓｆｕ＝１０－２２Ｗ／ｍ２Ｈｚ）,日面平均亮温度为９６３２Ｋ,径向亮温度分布,在日面光学边缘内侧０．９３６－０．９９２Ｒ处,存在临边增亮,平均增亮幅度相对于日面中心为９．７％． 相似文献
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辉耀动人的世纪天文大观─—喜迎１９９７年３月９日全食王玉卿随着月球逐渐遮住耀眼的太阳，整个天空越来越趋于昏暗，此时处于全食带地区的温度明显下降了五六度。然而．对身处这种特殊气氛下的人们来说，兴奋的情绪异常高涨，而且在太阳的最后一道光线消失时达到顶点，... 相似文献
11.
Air temperature and wind measurements on the surface and in the free atmosphere taken during the total solar eclipse of July 11, 1991, are analyzed. Surface air temperature decreased significantly, 2 to 5 °C in general, with the lowest values occurring 10 to 30 minutes after totality. In some places, surface wind speed decreased gradually during the eclipse, as a result of the decrease of air temperature and temperature gradients. In other places, it increased due to local atmospheric conditions. A radiosonde launched at 13:26 LT (local time) appeared to have been affected by the moon's shadow at about 13 km height. At this altitude temperature was relatively lower than usual and the balloon carrying the radiosonde experienced an upward acceleration. Also at this altitude wind direction changed and wind speed decreased 相似文献
12.
Shadia Rifai Habbal 《Astrophysics and Space Science》1996,243(1):49-56
The temperature in the acceleration region of the solar wind remains one of the most elusive parameters to measure. Knowledge of the temperature as well as its gradient in the inner corona is fundamental for placing constraints on physical mechanisms thought to be responsible for the coronal heating process, as well as for understanding the flow properties of the solar wind. Estimates of the helium abundance is essential for understanding the puzzling behavior of heavier ions in the solar wind. As an illustration of the difficulties and uncertainties involved in the inferences of plasma parameters in the wolar wind acceleration region, The inference of electron temperature and helium abundance will be described. Prospects for future observations will be briefly discussed. 相似文献
13.
为了充分利用Dome A地区绝佳的视宁度条件, 计划将南极望远镜安装在15m高的塔架上并使用轻质膜圆顶. 研究了在塔架和膜圆顶作用下风载对望远镜观测环境的影 响, 利用计算流体力学(Computational Fluid Dynamics, CFD)分析了在10m·s-1稳态风作用下,不同风向角、方位轴转动角以及镜筒转动角时,望远镜周围风速、湍动能的分布情况以及光程差的变化,同时研究了风屏对风速、湍动能的改善作用和带来的温升.结果表明,塔架和圆顶周围的风速与湍动能分布对风向的改变不敏感;迎风状态时望远镜附近的湍流分布与风速分布情况整体优于背风状态;当风速为10m·s-1时,在距离风屏1m远、3m高的位置处风速降为来流风速的1/3至1/4,望远镜附近的平均温升值为0.044 K. 相似文献
14.
Proton heating at stream interaction regions in the solar wind is investigated based on the solar wind data obtained by Suisei spacecraft between 0.68 and 1.01 AU from the Sun. The deflection angle of the solar wind flow in the ecliptic plane is used to identify the interaction region. In the solar wind flows coming from east of the Sun in low-speed streams and coming from west in high-speed streams, the radial gradient of proton temperature is flattened owing to heating in the interaction region. From comparison of the best-fitted power law dependence of proton temperature on the radial distance in the deflected flow with that in the non-deflected flow, it is suggested that heating in the interaction regions starts around 0.6–0.7 AU from the Sun. 相似文献
15.
S. Grzedzielski 《Planetary and Space Science》1980,28(8):799-802
Solar wind interaction with neutral interstellar helium focused by the Sun's gravity in the downwind solar cavity is discussed in a hydrodynamical approach. Upon ionization the helium atoms “picked up” by the (single fluid) solar wind plasma cause a slight decrease in the wind speed and a corresponding marked temperature increase. For neutral helium density outside the cavity nHe∞ = 0.01 atoms cm?3 and for interstellar kinetic temperature THe= 10,000 K, the reduction is speed of the solar wind on the downwind axis at 10 AU from the Sun amounts to about 2kms?1; the solar wind temperature excess attains 7000 K. The resulting pressure excess leads to a non-radial flow of the order of 0.25 km s?1. The possibility of experimental confirmation is discussed. 相似文献
16.
Correlation analysis of solar wind parameters, namely solar wind velocity, pro- ton density, proton temperature and mean interplanetary magnetic field (IMF) from the ACE spacecraft data near Earth, was done. To our best knowledge, this study is a novel one since we consider here only the parameters inside the solar wind, including the mean IMF and, hence, the solar wind is a self consistent system. We have proposed a Multiple Linear Regression (MLR) model for the prediction of the response variable (solar wind velocity) using the parameters proton density, proton temperature and mean IMF mea- sured as dally averages. About 60% of the observed value can be predicted using this model. It is shown that, in general, the correlation between solar wind parameters is sig- nificant. A deviation from the prediction at the solar maximum is interpreted. These results are verified by a graphical method. 相似文献
17.
Spectral gravity wave parameterization suitable for planetary thermospheres applied to wind and temperature from Mars Climate Database reveals enormously strong drag incompatible with the wind distribution. It points out to a possible wind reversal in the 110-140 km layer similar to the one in the Earth’s lower thermosphere. 相似文献
18.
Li-Xin Li 《Monthly notices of the Royal Astronomical Society》2007,375(1):240-256
Recently, a soft blackbody component was observed in the early X-ray afterglow of GRB 060218, which was interpreted as shock breakout from the thick wind of the progenitor Wolf–Rayet (WR) star of the underlying Type Ic supernova 2006aj. In this paper, we present a simple model for computing the characteristic quantities (including energy, temperature and time duration) for the transient event from the shock breakout in Type Ibc supernovae produced by the core-collapse of WR stars surrounded by dense winds. In contrast to the case of a star without a strong wind, the shock breakout occurs in the wind region rather than inside the star, caused by the large optical depth in the wind. We find that, for the case of a WR star with a dense wind, the total energy of the radiation generated by the supernova shock breakout is larger than that in the case of the same star without a wind by a factor of >10. The temperature can be either hotter or colder, depending on the wind parameters. The time duration is larger caused by the increase in the effective radius of the star due to the presence of a thick wind. Then, we apply the model to GRB 060218/SN 2006aj. We show that, to explain both the temperature and the total energy of the blackbody component observed in GRB 060218 by the shock breakout, the progenitor WR star has to have an unrealistically large core radius (the radius at optical depth of 20), larger than 100 R⊙ . In spite of this disappointing result, our model is expected to have important applications to the observations on Type Ibc supernovae in which the detection of shock breakout will provide important clues to the progenitors of Type Ibc supernovae. 相似文献
19.
Temperature and wind measurements extending up to 95 km have been made with rocket-grenade experiments at Natal, Brasil. On many occasions the temperature and wind speed above 60 km show uniformly spaced maxima and minima. In one series of these experiments four rockets were launched during a period of 18 hr. A comparison of these spaced observations gives an indication of the propagating character of the maxima and minima and also suggests a downward phase propagation. The perturbations in the temperature and the wind speed are similar in form but they appear to differ in phase. The wavelike appearance of the temperature profiles is believed to be caused by the adiabatic heating and cooling associated with propagating gravity waves. The wavelength obtained from these observations is 10–12 km which coincides with the expected vertical wavelength of 12 km for the dominant gravity wave in this altitude range. The observed temperature variations are also in agreement with the computed values for the prevailing conditions. 相似文献
20.
《Planetary and Space Science》2007,55(13):1990-2009
This study aims at interpreting the zonal and meridional wind in Titan's troposphere measured by the Huygens probe by means of a general circulation model. The numerical simulation elucidates the relative importance of the seasonal variation in the Hadley circulation and Saturn's gravitational tide in affecting the actual wind profile. The observed reversal of the zonal wind at two altitudes in the lower troposphere can be reproduced with this model only if the near-surface temperature profile is asymmetric about the equator and substantial seasonal redistribution of angular momentum by the variable Hadley circulation takes place. The meridional wind near the surface is mainly caused by the meridional pressure gradient and is thus a manifestation of the Hadley circulation. Southward meridional wind in the PBL (planetary boundary layer) is consistent with the near-surface temperature at the equator being lower than at mid southern latitudes. Even small changes in the radiative heating profile in the troposphere can substantially affect the mean zonal and meridional wind including their direction. Saturn's gravitational tide is rather weak at the Huygens site due to the proximity to the equator, and does not clearly manifest itself in the instantaneous vertical profile of wind. Nevertheless, the simulated descent trajectory is more consistent with the observation if the tide is present. Because of a different force balance in Titan's atmosphere from terrestrial conditions, PBL-specific wind systems like on Earth are unlikely to exist on Titan. 相似文献