ITU-R REPORT F 2061-2006 HF fixed radiocommunications systems《高频固定无线电通信系统》.pdf
《ITU-R REPORT F 2061-2006 HF fixed radiocommunications systems《高频固定无线电通信系统》.pdf》由会员分享,可在线阅读,更多相关《ITU-R REPORT F 2061-2006 HF fixed radiocommunications systems《高频固定无线电通信系统》.pdf(12页珍藏版)》请在麦多课文档分享上搜索。
1、 Rep. ITU-R F.2061 1 REPORT ITU-R F.2061 HF fixed radiocommunications systems (2006) 1 Introduction HF system emissions can be categorized as adaptive and non-adaptive. Non-adaptive systems depend on operator training and skill level to assess propagation variables and interference to find a clear,
2、reliable channel. Adaptive systems automate this process. Although adaptive systems have many advantages, including decreased operator training, non-adaptive systems will continue to be operated in the foreseeable future. There is potential for interference between these two types of systems. The em
3、ission characteristics of adaptive and non-adaptive systems require separate sets of characteristics data to enable accurate electromagnetic compatibility analysis in a given environment. Modern communications in the HF band also have specific attributes that make a viable solution for many emergenc
4、y response requirements. HF systems and networks provide a highly versatile means of communications to a broad base of users engaged in public protection and humanitarian efforts. Such systems can also bring inexpensive and reliable equipment to remote and lightly populated areas. In the event of th
5、e collapse of normal telecommunication operation due to natural disasters (e.g. earthquakes) and other emergencies, MF/HF systems could be established in a very short period of time to provide the emergency links required, in the first phase of the alarm or during the coordination of the relief oper
6、ation. 2 Non-adaptive systems 2.1 Introduction In the manual non-adaptive operational procedure, the operator must adjust the parameters of the system for maximum performance by monitoring the conditions of the ionosphere, tracking the variable propagation conditions, and selecting the operating con
7、ditions (i.e. primarily the frequency) that will allow the signal to propagate best. There is extreme variability and unpredictability, in the short term, of the HF propagation environment. Propagation in this band is primarily by the sky-wave mode, utilizing refraction of radio waves from the ionos
8、phere, or in some cases by the surface-wave mode. 2.2 Propagation The ionosphere, and radiowave propagation using it, are described in the ITU-R Handbook “The ionosphere and its effects on radiowave propagation” and in relevant Recommendations in the ITU-R P-Series (ITU-R P.368, ITU-R P.369, ITU-R P
9、.371, ITU-R P.434, ITU-R P.531, ITU-R P.532, ITU-R P.533, ITU-R P.534, ITU-R P.535). Some additional information may be found in the ITU-R Handbooks “HF broadcasting system design” and “Frequency adaptive communications systems and networks in the MF/HF bands”. In brief, the ionosphere is formed in
10、the Earths upper atmosphere, at heights above about 80 km, by the effects of ionizing radiation from the sun. The height and density of the ionization depend upon 2 Rep. ITU-R F.2061 the incoming radiation, the atmospheric constituents and their variation with height, etc. the Earths magnetic field
11、and the circulation of the upper atmosphere. The incoming solar radiation generally varies with the solar activity cycle, which has a period of approximately 11 years duration, as seen for example in the number of spots on the Suns surface. The incoming radiation ionizes a part of the upper atmosphe
12、ric gases and the resulting free electrons form the ionosphere, which has the property of refracting or reflecting radio waves. In the lower parts of the ionosphere the free electrons have a limited life-time before recombining, and the density of ionization varies approximately with the elevation a
13、ngle of the sun. These lower parts of the ionosphere are called the D and E regions or layers. Higher in the ionosphere, in the F region, electrons have a longer life-time and the ionization density is also strongly affected by winds and by the presence of the Earths magnetic field. The maximum freq
14、uency, which can be reflected vertically from an ionospheric layer depends on the ionization density and is called the critical frequency. The ionization density, and thus the critical frequency, depends on the geographical location and solar angle, and is subject to hour to hour, day to day and sea
15、sonal variability due to changes in the solar radiation, the solar-terrestrial environment, the upper atmospheric winds and the Earths magnetic field. The lower parts of the ionosphere also attenuate radio signals, while interaction with the Earths magnetic field also changes the signal polarization
16、. Terrestrial propagation may be considered as oblique incidence reflection from the ionospheric layers and additional propagation modes may have multiple reflections from the ionosphere and the Earths surface. The maximum frequency of propagation for each mode depends on the critical frequency and
17、on the elevation angle at the reflecting layer. Thus in general the received signal will comprise several modes, each with a different and variable strength; time of arrival and polarization. These longer term variations in propagation conditions, from hour to hour, day to day, with season and with
18、the solar cycle are predictable on a statistical basis. Prediction methods are available using Recommendation ITU-R P.533 or a variety of other methods. Such long-term prediction methods cannot give a precise estimate of the best frequency to be used at a specific date and time on a specific radio p
19、ath. Traditionally it has been the practice to use a frequency somewhat below the predicted maximum usable frequency (MUF), so as to ensure that a satisfactory signal would be received on most days of the month. A planned schedule of frequency changes through the day would be prepared for each month
20、, so as to maintain usable communications. The radio operator managing the circuit would use these frequency schedules, together with his experience and actual conditions on the day, and select the best frequency from the limited set available, thus managing the circuit operation on a minute-to-minu
21、te basis. The long-term predictions also give information on the active propagation modes and the elevation angles required for the antenna radiation. The ground wave propagation mode is stable and predictable. It is described in Recommendation ITU-R P.368 and a prediction method is available in sof
22、tware on the ITU-R website. At HF, the mode is only significant at ranges of up to several hundred kilometres over sea, and to substantially shorter ranges over land, in the lower part of the frequency range. Nevertheless, in appropriate circumstances the mode may be important. Circuit operation is
23、subject to these propagation modes, to the longer term ionospheric variations, to intensity and polarization fading. However, there are other short term and largely unpredictable factors, which are important. In the lower part of the ionosphere, at about 100 km, additional ionization may occur, in a
24、 manner which cannot be adequately predicted, due to meteorological factors and trace elements, and due to Rep. ITU-R F.2061 3 other mechanisms at both high and equatorial latitudes. This “sporadic-E” ionization may have a major impact on radiowave propagation and may provide an additional propagati
- 1.请仔细阅读文档,确保文档完整性,对于不预览、不比对内容而直接下载带来的问题本站不予受理。
- 2.下载的文档,不会出现我们的网址水印。
- 3、该文档所得收入(下载+内容+预览)归上传者、原创作者;如果您是本文档原作者,请点此认领!既往收益都归您。
下载文档到电脑,查找使用更方便
10000 积分 0人已下载
下载 | 加入VIP,交流精品资源 |
- 配套讲稿:
如PPT文件的首页显示word图标,表示该PPT已包含配套word讲稿。双击word图标可打开word文档。
- 特殊限制:
部分文档作品中含有的国旗、国徽等图片,仅作为作品整体效果示例展示,禁止商用。设计者仅对作品中独创性部分享有著作权。
- 关 键 词:
- ITURREPORTF20612006HFFIXEDRADIOCOMMUNICATIONSSYSTEMS 高频 固定 无线电通信 系统 PDF

链接地址:http://www.mydoc123.com/p-792931.html