ASHRAE 4735-2004 Study of Typical Meteorological Years and Their Effect on Building Energy and Renewable Energy Simulations《典型气象年及其对建筑节能和可再生能源的模拟的研究》.pdf
《ASHRAE 4735-2004 Study of Typical Meteorological Years and Their Effect on Building Energy and Renewable Energy Simulations《典型气象年及其对建筑节能和可再生能源的模拟的研究》.pdf》由会员分享,可在线阅读,更多相关《ASHRAE 4735-2004 Study of Typical Meteorological Years and Their Effect on Building Energy and Renewable Energy Simulations《典型气象年及其对建筑节能和可再生能源的模拟的研究》.pdf(8页珍藏版)》请在麦多课文档分享上搜索。
1、4735 Study of Typical Meteorological Years and Their Effect on Building Energy and Renewable Energy Simulations H. Yang, Ph.D. Member ASHRAE ABSTRACT This paper investigates the generation of typical meteo- rologicalyears (TMY) and example weatheryears (EWs) for Hong Kong, and studies their efects o
2、n the simulation results of the performance of building energy and renewable energy systems, i.e., solar andwindenergysystems. According to vari- ous methodologies, dijerent TMYs and EWYs were calculated using Hong Kongs weather data from the past 22 years. The results were used for a building energ
3、y simulation andfor a hybrid solar-wind energy simulation, as two case studies, to study their efect on the simulation results. To validate the eflect, deviations of thesimulation results fordiferent methods were compared. The results show that the diference could be very sgnijcant: -20% for hybrid
4、solar-wind enew systems and a relatively smaller diference for building energy systems, *5%. A larger error was produced by using EWYs compared with TMYs for both the building energy simulation and the hybrid solar-wind energy simulation. This proves that gener- ating the right TMY is important for
5、meeting different needs and various application systems. INTRODUCTION The performance of environmentally driven systems, such as HVAC systems, solar thermal systems, solar power systems, greenhouses, and wind generators, is dependent on weather variables such as solar radiation, dry-bulb tempera- tu
6、re, wet-bulb temperature, wind speed, etc. However, these variables are neither completely random nor deterministic. In order to simulate the energy performance of an existing system or predict the energy performance of a new system during the design stage, suitable representative weather data are r
7、equired. Here is where the concept of a typical meteorological year L. Lu (TMY) comes in. A TMY provides a standard for hourly data on solar radiation and other meteorological parameters for a period of one year, representing climatic conditions consid- ered typical over a long period of time. The p
8、roperties of a TMY include: (1) the meteorological measures of the TMY (Le., solar radiation, temperature, and wind speed) should have frequency distributions that are “close” to long-term distributions; (2) the sequences of the daily measures for the TMY should in some sense be like the sequences o
9、ften regis- tered at a given location, which is often referred to persistent structure; and (3) the relationships among the different measures for the TMY should be like the relationships observed in nature. The most popular method for deriving TMY, first devel- oped by Hall et al. (1 979), is an em
10、pirical approach selecting individual months from different years using the Filkenstein- Schafer (FS) statistical method (Filkenstein and Schafer 1971). The final selection involved examining statistics and the persistent structure of daily dry-bulb temperatures and daily total global solar radiatio
11、n. Other studies (Pissimanis et al. 1988; Lam et al. 1996; Petrakis et al. 1998; Merter and Arif 2000; Zhang et al. 2002; Thevenard and Brunger 2002a, 2002b) derived TMYs for different cities. In these studies, different weighting factors of meteorological parameters were considered, while the persi
12、stent structure of weather data was neglected. Considering higher weighting factors of total solar radiation and dry-bulb temperature, the results from these studies are suitable for building energy simulations. But the persistent structure of weather data has to be considered in assessing solar ene
13、rgy systems. The above results are not suit- able for wind energy systems because they have little to do with wind. Lu and Yang (2002) developed the TMY for Hong H. Yang is an associate professor and L. Lu is a Ph.D. student in the Department of Building Services Engineering, The Hong Kong Polytechn
14、ic University, Hong Kong. 424 Q2004 ASHRAE. Kong, which can be used to assess applications of solar and wind energy. Their work also proved that determining proper weather parameters and their weighting factors is imperative during the development of TMY for different kinds of systems. TO study the
15、effect of differently developed typical mete- orological years and example weather years (Wong and Ngan 1993) on simulation results or assessment results, typical meteorological years and example weather years for Hong Kong were developed using different weighting factors of meteorological parameter
16、s as proposed by different refer- ences. With the derived TMYs and Ems, two case studies, namely, on building energy simulations and solar-wind hybrid systems (renewable energy), were established to find out the effect. Huang (1 998) studied the impact of different weather data on simulated resident
17、ial heating and cooling loads in some cities or locations ofthe U.S., using differently developedtypi- cal weather year data. In Hong Kong, two kinds of typical weather year data, namely, a typical meteorological year (Lam et al. 1996) and an example weather year (Wong and Ngan 1993), have been deve
18、loped for building energy simulations. According to their different weather parameters and weighting factors, the developed TMYs and EWYs are different, which affects the results of system simulations or assessments. This study considers the impact of different TMYs and EWYs on building energy simul
19、ations and solar-wind hybrid energy system assessments. DEVELOPMENT OF EXAMPLE WEATHER YEAR (EWY) AND TYPICAL METEOROLOGICAL YEAR (TMY) Methodology The Finkelstein-Schafer (FS) statistical method is usually used to compose TMYs and EWYs to achieve close perfor- mance of frequency distribution betwee
20、n past weather data and statistical data by comparing the monthly or yearly prob- ability of distribution function (PDF) with the long-term PDF in the month or year concerned. Considering the characteris- tics of renewable energy systems, four weather parameter indices are cited, namely, dry-bulb te
21、mperature, dew-point temperature, wind speed, and global solar radiation. Here, the hourly indices are compared by their distribution function, not by their maximum, minimum, andmean functions. The month or the year with minimum weighting sum (WS) value should be the optimal TMY month or EWY year in
22、 terms of close frequency distribution. The FS statistics are determined by M 1 WS(y,m) = - M WFjxFSj j=l 1 wq=lJ j= 1 M FS(j,m) statistics for the jth parameter of index 2j O, means the candidate year and m the candidate month) monthly (m) PDF value atX(i) value for the jth parameter index in the y
23、ear y monthly (m) long-term PDF value at X(i) value for the jth parameter index total number of different4 values, which is determined by the index values starting point, ending point, and increasing interval; for different indices, N is different according to relative requirements number of the hou
24、rly weather parameter indices, M = 4 average weighted sum for the month m in the year y weighting factor for the jth parameter The weighting factors are crucial for choosing TMY and EWY data from past weather data. According to five different criteria-namely, from Hall et al. (1979) Hall, Marion and
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