PROPOSAL OF SEVEN-DAY DESIGN WEATHER DATA FOR HVAC PEAK LOAD CALCULATION

Similar documents
Taking the garbage out of energy modeling through calibration

Generation of an Annual Typical Meteorological Solar Radiation for Armidale NSWAustralia

Institut national des sciences appliquées de Strasbourg GENIE CLIMATIQUE ET ENERGETIQUE APPENDICES

Champaign-Urbana 1999 Annual Weather Summary

The Climate of Payne County

The Climate of Marshall County

Chapter 3. Regression-Based Models for Developing Commercial Demand Characteristics Investigation

Climate impact on seasonal patterns of diarrhea diseases in Tropical area

The Climate of Texas County

Champaign-Urbana 2000 Annual Weather Summary

The Climate of Kiowa County

The Climate of Bryan County

The Climate of Murray County

The Climate of Haskell County

Range Cattle Research and Education Center January CLIMATOLOGICAL REPORT 2012 Range Cattle Research and Education Center.

Champaign-Urbana 2001 Annual Weather Summary

The Climate of Seminole County

Drought in Southeast Colorado

ANALYSIS OF THE MICROCLIMATE OF SÃO CRISTÓVÃO AND ITS INFLUENCE IN HEATING SYSTEMS, VENTILATING AND AIR CONDITIONING (HVAC)

The Effect of Cloudy Days on the Annual Typical Meteorological Solar Radiation for Armidale NSW, Australia

EVALUATION OF ALGORITHM PERFORMANCE 2012/13 GAS YEAR SCALING FACTOR AND WEATHER CORRECTION FACTOR

A summary of the weather year based on data from the Zumwalt weather station

Agricultural Science Climatology Semester 2, Anne Green / Richard Thompson

The Climate of Grady County

The Climate of Pontotoc County

INFLUENCE OF THE AVERAGING PERIOD IN AIR TEMPERATURE MEASUREMENT

Memo. I. Executive Summary. II. ALERT Data Source. III. General System-Wide Reporting Summary. Date: January 26, 2009 To: From: Subject:

Range Cattle Research and Education Center January CLIMATOLOGICAL REPORT 2016 Range Cattle Research and Education Center.

Meteorology. Circle the letter that corresponds to the correct answer

Comparison of meteorological data from different sources for Bishkek city, Kyrgyzstan

Champaign-Urbana 1998 Annual Weather Summary

DEVELOPMENT OF COOLING LOAD TEMPERATURE DIFFERENTIAL VALUES FOR BUILDING ENVELOPES IN THAILAND

Radio Acoustic Sounding in Urban Meteorological Observations

Case Study Las Vegas, Nevada By: Susan Farkas Chika Nakazawa Simona Tamutyte Zhi-ya Wu AAE/AAL 330 Design with Climate

STUDY ON THE THERMAL PERFORMANCE AND AIR DISTRIBUTION OF A DISPLACEMENT VENTILATION SYSTEM FOR LARGE SPACE APPLICATION

Constructing a typical meteorological year -TMY for Voinesti fruit trees region and the effects of global warming on the orchard ecosystem

JOURNAL OF INTERNATIONAL ACADEMIC RESEARCH FOR MULTIDISCIPLINARY Impact Factor 1.393, ISSN: , Volume 2, Issue 4, May 2014

peak half-hourly New South Wales

Wind Resource Data Summary Cotal Area, Guam Data Summary and Transmittal for December 2011

November 2018 Weather Summary West Central Research and Outreach Center Morris, MN

peak half-hourly Tasmania

Interannual variation of MODIS NDVI in Lake Taihu and its relation to climate in submerged macrophyte region

Experimental and Theoretical Study on the Optimal Tilt Angle of Photovoltaic Panels

Winter Thermal Comfort in 19 th Century Traditional Buildings of the Town of Florina, in North-Western Greece

PREDICTING OVERHEATING RISK IN HOMES

8.1 Attachment 1: Ambient Weather Conditions at Jervoise Bay, Cockburn Sound

Direct Normal Radiation from Global Radiation for Indian Stations

A Typical Meteorological Year for Energy Simulations in Hamilton, New Zealand

Drought Characterization. Examination of Extreme Precipitation Events

OPTIMIZATION OF GLOBAL SOLAR RADIATION OF TILT ANGLE FOR SOLAR PANELS, LOCATION: OUARGLA, ALGERIA

WHEN IS IT EVER GOING TO RAIN? Table of Average Annual Rainfall and Rainfall For Selected Arizona Cities

Multivariate Regression Model Results

CLIMATOLOGICAL REPORT 2002

P7.7 A CLIMATOLOGICAL STUDY OF CLOUD TO GROUND LIGHTNING STRIKES IN THE VICINITY OF KENNEDY SPACE CENTER, FLORIDA

Chapter 2 Available Solar Radiation

Mountain View Community Shuttle Monthly Operations Report

Study on Thermal Load Calculation for Ceiling Radiant Cooling Panel System

Additional Wind and Stability Observations at S6mastaoageroi in Reyoarfiorour Il

Average Weather For Coeur d'alene, Idaho, USA

February 10, Mr. Jeff Smith, Chairman Imperial Valley Water Authority E County Road 1000 N Easton, IL Dear Chairman Smith:

2018 Annual Review of Availability Assessment Hours

OVERVIEW OF IMPROVED USE OF RS INDICATORS AT INAM. Domingos Mosquito Patricio

Monthly Long Range Weather Commentary Issued: February 15, 2015 Steven A. Root, CCM, President/CEO

A nalysis and Estimation of Tourism Climatic Index (TCI) and Temperature-Humidity Index (THI) in Dezfoul

Evaluation of monthly total global and diffuse solar radiation in Ibi, Taraba state, Nigeria

CLIMATE OVERVIEW. Thunder Bay Climate Overview Page 1 of 5

Tornado Hazard Risk Analysis: A Report for Rutherford County Emergency Management Agency

Generation of an Annual Typical Meteorological Solar Irradiance on Tilted Surfaces for Armidale NSW,Australia

Analysis of meteorological measurements made over three rainy seasons in Sinazongwe District, Zambia.

2013 Summer Weather Outlook. Temperatures, Precipitation, Drought, Hurricanes and why we care

Exercise 6. Solar Panel Orientation EXERCISE OBJECTIVE DISCUSSION OUTLINE. Introduction to the importance of solar panel orientation DISCUSSION

Chiang Rai Province CC Threat overview AAS1109 Mekong ARCC

Solar photovoltaic energy production comparison of east, west, south-facing and tracked arrays

Average Monthly Solar Radiations At Various Places Of North East India

Significant Rainfall and Peak Sustained Wind Estimates For Downtown San Francisco

Changing Hydrology under a Changing Climate for a Coastal Plain Watershed

Variability of Reference Evapotranspiration Across Nebraska

Development and performance evaluation of a methodology, based on distributed computing, for speeding EnergyPlus simulation

Will a warmer world change Queensland s rainfall?

STATISTICAL FORECASTING and SEASONALITY (M. E. Ippolito; )

Central Ohio Air Quality End of Season Report. 111 Liberty Street, Suite 100 Columbus, OH Mid-Ohio Regional Planning Commission

Life Cycle of Convective Systems over Western Colombia

Project No India Basin Shadow Study San Francisco, California, USA

Colorado s 2003 Moisture Outlook

Sierra Weather and Climate Update

Fire Weather Drivers, Seasonal Outlook and Climate Change. Steven McGibbony, Severe Weather Manager Victoria Region Friday 9 October 2015

Laboratory Exercise #7 - Introduction to Atmospheric Science: The Seasons

DAILY QUESTIONS 28 TH JUNE 18 REASONING - CALENDAR

330: Daytime urban heat island intensity in London during the winter season

Estimation of Diffuse Solar Radiation for Yola, Adamawa State, North- Eastern, Nigeria

Causes of high PM 10 values measured in Denmark in 2006

Local Ctimatotogical Data Summary White Hall, Illinois

Chapter-3 GEOGRAPHICAL LOCATION, CLIMATE AND SOIL CHARACTERISTICS OF THE STUDY SITE

DROUGHT IN MAINLAND PORTUGAL

Supplementary Figure 1 Annual number of F0-F5 (grey) and F2-F5 (black) tornado observations over 30 years ( ) for Canada and United States.

Marche Region Climate Analysis by Danilo Tognetti 1

September 2018 Weather Summary West Central Research and Outreach Center Morris, MN

not for commercial-scale installations. Thus, there is a need to study the effects of snow on

AN EVALUATIVE METHOD FOR HIGH-PERFORMANCE WINDOW SYSTEM AND WINDOW SIDE RADIATION ENVIRONMENT

Analysis of Rainfall and Other Weather Parameters under Climatic Variability of Parbhani ( )

Transcription:

Ninth International IBPSA Conference Montréal, Canada August 5-8, PROPOSAL OF SEVEN-DAY DESIGN WEATHER DATA FOR HVAC PEAK LOAD CALCULATION Hisaya ISHINO Faculty of Urban Environmental Sciences, Metropolitan University,, Japan ishino@ecomp.metro-u.ac.jp ABSTRACT This paper proposes a method for creating an extreme seven-day set for HVAC design purposes and examines its suitability. The method involves reviewing data from 2 years of weather observations and selecting a seven-day period during which the weather conditions were extreme. The dry-bulb temperature, the humidity ratio, the solar radiation and other weather elements were obtained for one-hour intervals during the selected period as the design weather conditions. In order to select a meteorologically extreme period with distinct weather characteristics, two weather indices were used. The extremity of the design was evaluated by determining both the frequency of occurrence of characteristic weather values and the likelihood of the thermal load exceeding the design peak load, which was calculated using the design. The results confirmed the validity of using the data to determine sufficient capacities for HVAC equipment. INTRODUCTION In the past, used for HVAC design in Japan has been determined by taking the weather values over the previous ten years or so, and then carrying out statistical processing to extract extreme values for each weather element and time category (SHASE, 2). These values are then linked and used as one-day design. However, this design represents unrealistically severe weather, and can lead to overestimation in the required equipment capacity. In the United States, to give the design weather conditions, an extreme value of a certain weather element was selected from among the weather observation values recorded over all time, and the other weather element values corresponding to that time were taken as a set (ASHRAE, 2). Colliver et al proposed a method for determining design weather sequences that uses the mean value for a certain weather element over a given period of time as an index in order to select several days of extreme weather (Colliver et al, 998). The real values for several weather elements during that period were then proposed for the design weather conditions. Although various types of design weather sequences that differ in the indices and length of the sequence used have been obtained, an individual must decide the sequence to be used. Based on the fact that the characteristics of the weather when the peak load occurs vary depending on the HVAC equipment, the author proposed a method in which several types of extreme-weather period are selected based on two weather indices. This allows for the selection of realistic weather with distinct characteristics and allows for a reduction in the number of types of design. The proposed method is for creation of seven-day design including weather elements required for design peak load calculation such as dry-bulb temperature, humidity ratio, normal direct solar radiation, horizontal diffuse solar radiation and horizontal nocturnal radiation. Weather can be affected by urban heat generation and exhausted gas and weather characteristics on holidays may be different from those on weekdays. Therefore, the design are provided for 7-day period matching the human weekly working cycle. METHOD OF CREATING DESIGN WEATHER DATA Data sources The data source is the expanded AMeDAS base (Akasaka et al, 23). This database comprised of 2 years (98-2) of data of primary weather elements for approximately 84 domestic locations in Japan. This paper employed the data for seven cities:,,,,, and. Weather type and weather indices A method for creating two types of for heating design and three types of for cooling design is proposed. The two types of for heating design are called the t-x data and the t-jh data. ) In the t-x data, the dry-bulb temperature (t) - 45 -

and the humidity ratio (x) are extreme. This design data is suitable for equipment such as air-handling units in which fresh air is introduced. For the weather indices, the mean dry-bulb temperature (tm) over a seven-day period is used as the first index, and the mean humidity ratio over a seven-day period (xm) is used as the second index. A seven-day period is selected over which both of these are extreme. 2) The t-jh data is taken from cloudy weather data with extreme dry-bulb temperatures and weak horizontal solar radiation (Jh). This is suitable for equipment such as air-handling units for perimeter zones with good sunlight. The mean dry-bulb temperature over seven days is used as the first index, and the mean value over seven days for the daily cumulative horizontal solar radiation (Jh, m) is used as the second index. The three types of used for cooling design are the h-t, Jc-t, and data. ) The h-t data is taken from humid weather data with extreme enthalpy (h) and dry-bulb temperature. This is suitable for devices such as airhandling units into which fresh air is introduced. The mean enthalpy (hm) over a seven-day period is used as the first index and the mean dry-bulb temperature over a seven-day period is used as the second index. 2) The design intention for the Jc-t data was to represent a period with a high level of ambient solar radiation and an extreme dry-bulb temperature around the outside perimeter of the building. This is suitable for devices such as an air-handling units used at a perimeter. The first index uses the mean value over a seven-day period for the daily cumulative solar radiation incident on the vertical side of a cylindrical surface (Jc, m), and the second index uses the mean value over a seven-day period for the dry-bulb temperature. 3) The data gives design for HVAC equipment in south-facing zones. The first index used the mean value over a seven-day period for the daily cumulative solar radiation incident on /4 of the south-facing side of a cylindrical surface (Jcs, m), and the second index used the mean value over a seven-day period for the dry-bulb temperature. Although there is a higher load on the air-handling unit for south-facing zones during autumn, the month in which the peak load occurs depends upon the building characteristics. For this reason, extreme weather from September and October was selected and used to create the two types of data. However, since the peak summer period is short in, August and September were selected as the extreme weather periods, and because the peak summer period is long in, October and November were selected as the extreme weather periods. Data Creation Procedure ) Ranking of the values of the first index For the heating design, the mean weather values were calculated over seven-day periods during the fourmonth period from December through March. For the cooling design, the mean weather values were calculated over seven-day periods during the fivemonth period from June through October (for, this was the six-month period from June through November). These mean values were ranked in order of extremity. The seven-day mean values were calculated for seven-day periods by shifting the value one day at a time. 2) Target value for the frequency of occurrence The target values for the frequency of occurrence were obtained for the first and second indices. The target value means the probability of occurrence of weather periods that have more extreme value of the first/second index than that for the selected period as the extreme-weather period. The frequency of occurrence of the weather values such as the first and second index is presented as the percentage value based on the number of all periods over 2 years that is 735 periods. This paper indicates the results based on a target frequency of occurrence of %. 3) Selecting the extreme-weather period For the t-x data, 3 periods (corresponding to.4% of the total number of periods over 2 years) were initially selected such that the frequency of occurrence of the first index was close to the target value. Next, out of these 3 periods, one period from both January and February was selected as the extreme-weather period such that the frequency of occurrence for the second index was close to the target value. For the t-jh data, 73 periods (corresponding to % of the total number of periods over 2 years) were selected using the first index, because there are fewer seven-day periods of cloudy weather. For the h-t and Jc-t data, 3 periods were selected for which the frequency of occurrence of the first index was close to the target value. Then, out of these 3 periods, one period from both July and August was selected as the extreme-weather period such that the frequency of occurrence of the second index was close to the target value. For the data, 3 periods were selected for which the frequency of occurrence of the first index was close to the target value from the specified month. Then, one period was selected for which the frequency of occurrence of the second index was close to the target value. As mentioned above, two months were specified for each city depending on the peak - 452 -

Figure Typical floor plan of an office building Table Simulation conditions Set points of space air temperature and relative humidity 26C and 5% in summer season from June through September 24C and 5% in spring season from April through May 22C and 5% in winter season from December through March 24C and 5% in autumn season from October through November Cooling and Heating hours from 7: to 8: in winter season (warming-up hours from 7: to 9:) from 8: to 8: in the other season (pulling-down hours from 8: to 9:) Ventilation Fresh airflow rate 4 CMH/m2 Ventilating hours from 9: to 8: Internal heat generation Lighting 2W/m2 Occupant.2 persons/m2 OA equipment W/m2, and : frequencies of occurrence of tm, xm and Jh,m tm: mean dry-bulb temperature over a 7-day period, xm: mean humidity ratio over a 7-day period Jh,m: mean value over a 7-day period for the daily cumulative horizontal solar radiation occurrence.. 4 5 6 7 8 9 Ranking for tm Figure 2 Frequencies of occurrence of weather characteristic values compared with ranking for the seven-day mean of dry-bulb temperature (tm) summer period. One extreme-weather period from each of these months was then selected. : August and September;,,, and : September and October; : October and November In the case of the h-t data that have the frequency of occurrence for each of the first and second index equal to the target value, the same design can be created even if enthalpy and temperature are changed with humidity ratio and temperature as the two weather indices. However, the frequency of occurrence for the first or second index is not always equal to the target value. Therefore, the important weather elements for the equipment were used as the index. 4) Weather elements for the design The dry-bulb temperature, humidity radio, total horizontal solar radiation, nocturnal radiation, and wind direction and velocity values at hourly intervals for the selected extreme-weather periods were presented as the design. EXAMINATION METHOD The severity of the proposed design weather was first examined from the standpoint of the frequency of occurrence for the weather characteristic values. Next, the dynamic thermal loads were calculated for the weekly periods used for the design weather data, and the design peak load obtained from calculation and likelihood of the thermal load exceeding the design peak load were evaluated. Calculation of the dynamic thermal load was performed using the New HASP/ACLD-β (Nagai et al., 24). In Japan, HVAC systems generally operate intermittently, and the peak heating load occurs during the warming-up time. This program performs calculations without the need to input the heating capacity based on the assumptions that the heating rate during the warming-up time is constant and that the room air temperature reaches the set point at precisely the time that warming-up finishes. Based on these assumptions, the design peak load can be determined for the heating equipment. These calculations were carried out for four directional zones on a typical floor in an office building, as shown in Fig.. Each zone is conditioned by each air-handling unit that introduces outside air for the zone. The calculation conditions are provided in Table. The likelihood of the thermal load exceeding the design peak load was determined using the rankings of the hourly thermal load calculated over 2 years with the expanded AMeDAS. RESULTS - 453 -

t g x g/k t C W/m2 Jh x g/kg 4 2 5 8 6 4 2 Jan. 2 986 4 2 Diffuse radiation 22 23 24 26 27 (a) The t-x design tm [C xm [g/kg hm J/g Jh,m MJ/m2day occurrence % 2 - -2 8 6 4 2 4 3 2-2. C W/m2 5 8 6 4 Diffuse radiation (a) The t-x design (b) The t-jh design Figure 4 Weather characteristic values and their frequencies of occurrence in two types of heating design Jh 2 Jan. 29 3 3 Feb. 2 3 4 99 (b) The t-jh design Figure 3 Fluctuation of dry-bulb temperature t, humidity ratio x and horizontal solar radiation Jh in two types of heating design Heating design First, examinations were conducted using the design data for. Fig. 2 shows the frequencies of occurrence,, and for tm, xm, hm and Jh, respectively, as a function of the ranking sequence based on the first index tm. The 73 periods from 37 to 9, which correspond to frequencies of occurrence between.5 to.5%, are indicated. There were many periods during which both and were around %, making it possible to select the t-x data with a frequency of occurrence of around % from the 3 periods from 58 to 87. On the other hand, there were few cases in which was around %, and selecting the t-jh with a frequency of occurrence of % required 73 periods from 37 to 9. The time fluctuations for the t-x and t-jh data for are shown in Fig. 3. The t-x data is characterized by clear days and a large daily variation in dry-bulb temperatures. In the t-jh data, on the other hand, the level of solar radiation is low and the daily variation in dry-bulb temperatures is small, while on many days the humidity was somewhat high. Two types of design could be created with vastly different weather characteristics. Fig. 4 shows the principal weather characteristic values for the t-x and t-jh data of the seven cities in Japan, along with their frequencies of occurrence. The t-x data for all cities is severe, with, and being around %, while ranges between 2 and 3%. Therefore, it was possible to create design with a similar degree of extremity. Although there were some cities in which the frequencies of occurrence of the first and second indices, and, were both close to the target of around % for the t-jh data, there were also cities such as and where was around 7% and the level of solar radiation was somewhat high. Cooling design Figs. 5 and 6 show the frequencies of occurrence for the weather characteristics for with rankings between 58 to 87 for hm and Jc,m, respectively. From Fig. 5, it can be seen that periods - 454 -

currence % oc Frequence of occurrence [%.... 6 65 7 75 8 85 Ranking f or hm FJc,m Figure 5 Frequencies of occurrence of weather characteristic values compared with ranking for the seven-day mean of enthalpy (hm) 6 65 7 75 8 85 Ranking f or Jc,m Figure 6 Frequencies of occurrence of weather characteristic values compared with ranking for the seven-day mean of daily cumulative solar radiation incident on a cylindrical surface (Jc,m) x g/kg Jh W/m2 t C x g/kg t C 24 2 6 35 3 8 6 4 2 Aug. 6 984 24 2 6 35 3 Diffuse radiation 7 8 9 2 2 22 (a) The h-t design in which both and are around % were selected from the 3 periods from 58 to 87. Similarly, Fig. 6 shows that periods can be selected in which both FJc,m and are around %. The time fluctuations in the h-t data and the Jc-t for are shown in Fig. 7. The Jc-t data reflects more consecutive days during which there was strong solar radiation. The differences observed in the dry-bulb temperature and humidity characteristics were not that significant between the two types of data. Fig. 8 shows the frequencies of occurrence for the weather characteristic values for with rankings between 58 to 87 for Jcs,m during the months of June through October. Most of the periods in this range were in October. The frequency of occurrence for the second index is 3 to 4%, and it was not possible to select a period within October that would produce the target value of %. Fig. 9 shows the time fluctuations in the data for September and October for. The solar radiation is the value for the south-facing surface. The dry-bulb temperature for the September design is fairly extreme, exceeding 3 o C on consecutive days. Both the dry-bulb temperature and the humidity are low in the October design, and the data includes cloudy days. The October data could possibly be used to study natural ventilation. Fig. shows the weather characteristic values Jh W/m2 8 6 4 2 Diffuse radiation Aug. 2 3 4 5 6 7 984 (b) The Jc-t design Figure 7 Fluctuation of dry-bulb temperature t, humidity ratio x and horizontal solar radiation Jh in two types of cooling design and their frequencies of occurrence for the four types of cooling design. In the results,,,, and of the Jc-t data are all around %. The data Jc-t was found to be more extreme than the h-t data from the viewpoints of horizontal solar radiation, dry-bulb temperature, and humidity. Fig. shows the frequencies of occurrence of the mean values over seven days for the daily cumulative solar radiation incident on the south-, west-, north- and east-facing surfaces for the four types of cooling design in. In the data, the frequency of occurrence for the solar radiation incident on the south-facing surface is the target value of % for October, but was 4% for September. In the Jc-t data, the frequencies of occurrence for solar radiation incident on the west-, north- and east-facing surfaces are around the target value of %, so the Jc-t data may be suitable for HVAC equipment in zones - 455 -

o x k g/ g 2 Js W/ ccurrence % t [C m g x [g/k t [C W/m2 Js.. 2 6 2 35 3 8 6 4 2 Sep. 5 6 7 8 9 994 (a) The design (Sep.) 2 8 3 2 5 8 6 4 2 6 65 7 75 8 85 Ranking f or Jcs,m Oct. 4 FJcs,m Total solar radiation 5 6 7 995 (b) The design (Oct.) Figure 9 Fluctuation of dry-bulb temperature t, humidity ratio x and solar radiation incident on a south-facing surface Js in two types of the cooling design weather data facing these three directions., Figure 8 Frequencies of occurrence of weather characteristic values compared with ranking for the seven-day mean of daily cumulative solar radiation incident on the south-facing side of a cylindrical surface Jcs,m 8 9 2 Fig. 2 shows the weather characteristic values and their frequencies of occurrence for the four types of tm C xm [g/kg hm J/g Jh,m MJ/m2day occurrence [% 4 3 2 2 9 8 7 6 5 4 3 2. h-t Jc-t (Sep.) Weather type Figure Weather characteristic values and their frequencies of occurrence in four types of cooling design occurrence of Jv,m [% 5 5. South cooling design for the seven cities. The results show that in the h-t data for and and in the Jc-t data for, the frequencies of occurrence of all of the weather characteristic values are around %. The h-t data may be sufficient for and without using the Jc-t data. Conversely, for, the design weather Jc-t data may be sufficient without using the h-t data. The and values for the Jc-t data are around % for all cities, with the exception of and, due to slightly high humidity. Design thermal peak load Fig. 3 shows the design peak load for the four directional zones in office buildings in determined using the design, as well as values for the likelihood of the thermal load West North Surface orientation (Oct.) Jv,m: Mean of the daily cumulative vertical radiation over 7 days (Oct.) (Sep.) Jc-t h-t East Figure Frequencies of occurrence of the seven-day mean of daily cumulative vertical solar radiation Jv,m - 456 -

C tm 4 35 3 2 xm [g/kg 2 5 hm J/g Jh,m Jc,m Jcs,m MJ/m2day 9 8 7 6 5 4 3 2 Jh,m Jc,m Jcs,m Jcs,m occurrence [%. FJc,m FJcs,m FJcs,m (a) The h-t design (b) The Jc-t design Figure 2 Weather characteristic values and their frequencies of occurrence in four types of cooling design for seven cities (c) The design (Aug. for, Oct. for and Sep. for the other cities) (d) The design (Sep. for, Nov. for and Oct. for the other cities) exceeding the design peak load. The likelihood of the thermal load exceeding the design peak load was determined using the rankings of the hourly thermal load. In this paper, the design peak load is regarded as sufficiently safe if the likelihood of the thermal load exceeding the design peak load is.% or less. The heating design peak load was higher in the south- and east-facing zones when the t-jh data was used, while in the west-facing zone the t-x data produced a larger load. The t-jh data tends to be suitable in zones that receive good sunlight and the t-x data tends to be suitable in zones that do not receive good sunlight. Also, the likelihood of the thermal load exceeding the design peak load for heating of was low in all zones, at around.%. The cooling design peak load was higher in the southfacing zone when the data from September was used. For the west- and east-facing zones, the difference in using the h-t and Jc-t data was not significant, while in the north-facing zone, the cooling design peak load was larger when the Jc-t data was used. From the perspective of the likelihood of the thermal load exceeding the design peak load, sufficiently valid results will generally be produced for all zones if the Jc-t design data is Design peak load W/m2 Likelihood of thermal load exceeding the design peak load [% used. 2 5 5. t-jh t-x t-x t-jh (Sep.) Oct. Jc-t h-t (Oct.) h-t. Jc-t (Sep.). South West North East SouthWest North East Zone Zone (a)heating dsign (b)cooling design peak load peak load Figure 3 Design peak loads and likelihood of thermal load exceeding the design peak load CONCLUSION Two types of for heating design and three types of for cooling design were - 457 -

proposed and evaluated. ) Using two weather indices, different types of real weather with clear differences in weather characteristics, such as t-x data and t-jh data, could be selected. 2) In some cities, the h-t data and Jc-t data had similar characteristics. Both these design weather data sets included extreme values for the enthalpy, drybulb temperature and solar radiation. 3) If the equipment capacity is determined from the maximum value of the design peak load in all of the design weather types, it will be possible to design HVAC equipment with a sufficient capacity. In the future, case studies will need to be conducted on a wider scale to clarify which type of design is appropriate for which type of HVAC equipment. NOMENCLATURE t = Dry-bulb temperature [ o C x = Humidity ratio [g/kg h = Enthalpy [J/g Jy = Solar radiation incident on a surface y[w y is as follows h = A horizontal surface c = A cylindrical surface cs = /4 of the south-facing side of a cylindrical surface s = A south-facing surface tm, xm, hm = Mean of t, x, h over 7 days Jy,m = Mean of the daily total of Jy over 7 days [MJ/m2day Fz = Annual cumulative frequency of occurrence of weather parameter z [% REFERENCES Akasaka, H. et al. 23. Expanded AMeDAS Weather Data, AIJ Japan ASHRAE. 2. 2 ASHRAE Handbook- Fundamentals. ASHRAE, Inc. Atlanta USA. Colliver, D. G., R. S. Gates et al. 998. Sequences of Extreme Temperature and Humidity for Design Calculations (RP-828). ASHRAE Transactions 4 (), USA. Nagai, T. and H. Ohga. 24. Features and User's Guide of New HASP/ACLD-B, Proceedings of SHASE Symposium 'The Present and the Future of Software for Thermal Load and HVAC', SHASE. Japan. SHASE. 2. Handbook of Heating, Air- Conditioning and Sanitary, Version 3, Vol.3. SHASE Japan - 458 -