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candidate action a, and all forms of RL entail both the exploitation of current knowledge and the exploration of the unknown. 11.2.3.1 Exploitation: Finding WTOP The <Self/> may be used as a schema-schema for knowledge action evolution by the exploitation of current knowledge via RL. Suppose a <User/> tunes to WTOP every morning. The AACR has a goal of enhancing <Information/> <Preferences/> of the <User/>, so it needs to know if the <User/> is expressing a <Preference/> by tuning to WTOP. One way for a CR to nd out is to ask. This can be a pain in the neck to the user and not very informative to the AACR. AACR: What are you doing with the radio <User/>: I m listening to it you dummy. AACR: No, I mean the channel. <User/>: You are the radio, why don t you know what channel AACR: Sorry, I know what channel but what information are you getting from that channel <User/>: I m driving so be quiet, will you This continues until the AACR is returned for a refund or there is a traf c accident and lawsuit. In a more focused exchange the CR monitors the <User/> <Tuning/> to FM channel 107.7 in <Location> Fairfax County, VA </Location> reading the channel s <Annotation> News </Annotation>. The ability to read the text annotations is declared in RXML to the <Self/> (Expression 11-7) as a <Sensor/> along the <Sense/> <Path/> from the <FM-Radio/> of the <Outside/> to the <Observations/> inside the <Self/>. Expression 11-7 Reading FM Captions

outage events and battery and PV sizing necessary to provide sustainable operation of the system. The simulator must take into account the inef ciencies caused by losses in the charge controller and other components in the system including the battery temperature ef ciency; for most battery families, as the ambient temperature decreases, the charge carriers within the battery become more sluggish and the battery capacity decreases signi cantly. Publicly available meteorological data are only available for horizontal and fully tracking (direct normal) components and cannot be used directly for a xed planar solar panel. For this reason it is necessary to develop a conversion methodology to compute the energy incident on the panel using the available datasets. The total radiation received by a panel consists of three terms: the direct component, Ic , which is the radiation coming directly from the sun; the diffuse component, Dc (due mainly to sky diffraction), which consists of non-direct-radiation components; nally the ground-re ected component, Rc , which is often neglected. Calculation of the direct component can be performed using well-known trigonometric calculations and is straightforward. On the other hand, the calculation of the diffuse component estimation requires a more complex conversion model, and several have appeared in the literature. Before examining the diffuse component estimation methodologies, let us rst discuss the data available in North American records [4, 5]. Generally, ve different solar radiation data elds are available. They are brie y discussed below.

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At first I didn t understand how it would be possible, since the standard carry trade done by hedge funds requires lines of credit with Japanese banks, or access to currency options and fancy formulas for figuring the future value of currencies I can t do any of that But I did find something on a retail platform that can t be used by a bank or a hedge fund And it might be even better Everyone now sat on the edge of their seat To them, this was better than a movie If I had told them I needed them each to sing the theme song from the Brady Bunch before I continued, they would have all broken into song What I found is that I don t need options I don t need futures contracts and I don t need lines of credit with Japanese banks.

Extraterrestrial Horizontal Radiation. This is the amount of solar radiation received on a horizontal surface at the top of the atmosphere. It is also known as topof-atmosphere (TOA) irradiance and is the amount of global horizontal radiation that a location on earth would receive if there were no atmosphere. This number is used as the reference amount against which actual solar energy measurements are compared.

<Skill> <FM-Listen> <Outside> <FM> <From> <RF> 88 <Units> MHz </Units> </RF> </From> <To> <RF> 108 <Units> MHz </Units> </RF> </To> </FM> </Outside> <Action> <Call> read-fm-text.dll <CMD-line> <RF/> = X </CMD-line> <Returns> <Observation> <FM/> = X <Audio-Stream Stream = S <Annotation> WTOP NEWS </Annotation> </Observation> </Returns> </Call> </Action> </ FM-Listen> </Skill> The channel to which the user is tuned has the text <Annotation/> WTOP NEWS. The CRA <Self/> lists News as an <Information/> <Service/> for

Extraterrestrial Direct Normal Radiation. This reading is the level of solar radiation received on a surface normal to the sun at the top of the atmosphere. The previous two elds are deterministic and can be calculated using the sun earth distance and position equations. The rest of the elds are random processes. In general, due to the motion of the earth around the sun and its rotation, solar insolation experiences cyclic changes over a year, and these variations are deterministic to a large extent. However, complex weather processes such as humidity, temperature, air pressure, and cloud type affect the received insolation. The following data is typically included.

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