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where d is the time in days from the vernal equinox. This is so because in one year of approximately 365.24 days the earth completes a 360 orbit around the sun. For a sun-synchronous orbit the local mean time must remain constant. The advantage of a sun-synchronous orbit for weather satellites and environmental satellites is that the each time the satellite passes over a given latitude, the lighting conditions will be approximately the same. Eq. (2.58) shows that for a given latitude and fixed inclination, the only variables are as and . In effect, the angle ( as) must be constant for a constant local mean time. Let 0 represent the right ascension of the ascending node at the vernal equinox and the time rate of change of then tSAT 1 c 15 1 c 15

The startsap command is really a UNIX alias (a symbolic name pointing to something else) that calls the needed start programs. To stop the system, enter stopsap in the command line. On Windows NT systems, you can start and stop R/3 from within the SAP Service Manager that is located on the NT Programs menu, within the SAP R3 programs group. The process of starting and stopping the system is explained in detail in the next chapter.

12 12 (2.60)

For this to be constant the coefficient of d must be zero, or r 360 365.24 0.9856 degrees/day (2.61)

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With release 4.0 or R/3, SAP introduced a new monitoring architecture within the CCMS based on advanced object oriented technology. The alert monitor 4.x is based on and developed using this new monitoring architecture. The 4.x alert monitor includes the following added features over previous 3.x releases: Dynamic generation of alerts on each system being monitored Assignment of analysis tools for different types of alerts or alarms Easy display, logging, and management of occurring alerts with a convenient alert browser Ability to adapt monitoring tools to system managers' requirements Ease of integration with external tools and applications using APIs and BAPIs Ability to manage alerts from several R/3 systems environments

Use is made of the regression of the nodes to achieve sun synchronicity. As shown in Sec. 2.8.1 by Eqs. (2.12) and (2.14), the rate of regression of the nodes and the direction are determined by the orbital elements

The new monitoring architecture, shown in Fig. 12 9, is made up of the following main components: Data suppliers. Data suppliers are programs that collect information from different parts or components of the R/3 systems and the related environment. Data suppliers keep information related to different Monitoring objects. Initially, the system includes active data suppliers for host systems where SAP is running, both application instances and database. Monitoring objects. These objects represent different elements or system components that can be monitored within R/3 or a related environment. Monitoring objects are created by data suppliers, which are also in charge of collecting information about the monitoring objects. Each type of information that can be collected for a monitoring object is known as an attribute. For example, a monitoring object can be swap space and its attribute space used, with a value of 10 percent, which is the data collected by the data supplier. Data consumers. These are programs that, depending on the monitoring object status, process the 434

Tiros-N Series Orbital Parameters 833-km orbit 870-km orbit 98.899 102.37 min 25.59 /day E 0.986 /day E 14.07

SOURCE:

Monitoring Tree object information collected from data suppliers. This information is used for management, monitoring, and analysis. Like the data suppliers, the data consumer programs are linked to monitoring objects using BAPIs, so they can be either R/3 or external programs.

a, e, and i. These can be selected to give the required regression of 0.9856 east per day. The orbital parameters for the Tiros-N satellites are listed in Table 2.5. These satellites follow near-circular, near-polar orbits.

2.11 Standard Time Local mean time is not suitable for civil time keeping purposes because it changes with longitude (and latitude), which would make it difficult to order day-to-day affairs. The approach taken internationally is to divide the world into 1-h time zones, the zonal meridians being 15 apart at the equator. The Greenwich meridian is used as zero reference and in the time zone that is 7.5 about the Greenwich meridian the civil time is the same as the GMT. Care must be taken, however, since in the spring the clocks are advanced by 1 h, leading to British summer time (BST), also known as daylight saving time. Thus BST is equal to GMT plus 1 h. In the first zone east of the GMT zone, the basic civil time is GMT + 1 h, and in the first zone west of the GMT zone, the basic civil time is GMT 1 h. One hour is added or subtracted for each additional zone east or west. Again, care must be taken to allow for summer time if it is in force (not all regions have the same summer time adjustment, and some regions may not use it at all). Also, in some instances the zonal meridians are adjusted where necessary to suit regional or country boundaries. Orbital elements are normally specified in relation to GMT (or as noted in Sec. 2.9.2, UTC), but results (such as times of equatorial crossings) usually need to be known in the standard time for the zone where observations are being made. Care must be taken therefore to allow for the zone change, and for daylight saving time if in force. Many useful time zone maps and other information can be obtained from the Internet through a general search for time zones.

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