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GEOGRAPHICAL REPORTS

OF TOKYO METROPOLITAN UNIVERSITY 43(2008)77−81

TOKYO WARDS−OBSERVATION RESULTS OF METROS一

      

       

Hitoshi YOKOYAMA,Haruo ANDO,Mika ICHINO,

      

      Koichiro ISHII and Takehiko mm

伽紬e曲an heat island phenomena血sunrmer over Tokyo WardS was stUdied by using

血e(lata obtained丘om METROS(Metropolitan Environmental Temperature and Rain制1

0bservation System), which is the high density heat island phenomena observation netWork. The observational resultS clarified the detailed spatial(listributions of temperature never known before.

Concerning血e spatial面s面buUon of(laily mar(imum temperature, the region wi血a relatively high temperature extendS fbom the centra1 Tokyo district toward the nonhern and nonhwestern

area. On出e other hand, relatively high values in the daily minimum tem卿ture are distributed around止e coastal area of Tokyo Bay including血e central Tokyo dis重㎡ct. Since 1血e cen加al Tokyo district has significantly high temperatures both in the daytime and in the nightdme, and also raises the temperature in the a(lj acent nonh and nonheast area, it is necessary to take countemieasures prefbrentially to this district.

Key words:heat island phenomena, Tokyo Wards, air temperature, days oftonid night, time         proportion ofhours which exceeded 30°C

1. introduction

  The high temperatUre wnh intensified heat island phenomena causes various negative impacts,

such as the辻【crease of heat stroke patientS, aggravalion of a廿pollution,㎞crease of local severe ra血, increase of energy consumption, and so on(Ministry of止e Environment 2005). On July 20,

2004,an extraordinarily high temperature of 39.5°C was recorded at Otemachi in Tokyo. PUblic concern about the heat island phenomena has been growing year by year. The Tokyo Metropolitan

Research lnsti加te for Environmental Protection(MRIEP)has tackled the heat island issues for supponing the planning of countermeasures ato et al.1994;Mi㎞li伽乙1997a,1997b;Ando et al.2003;Mikami et al. 2004;Yokoyama et al.2005). Tlien it became clear that detailed

observation data were necessary fbr the investigations of mechanism and cause of heat island

phenomena. However, since there are not enough meteorological stations by the Japan Meteorological Agency in the Tokyo area fbr the detailed analysis, the MRIEP started the spatiotemporally high−density meteorological observation system in cooperation with Tokyo Me噸litan University(㎜)丘om血e summer of 2002. It is called甑皿OS働opoli伽

Tokyo Metropolitan Research lnstitUte for Environmental ProteCtion

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Environmental Tempera加e and Rainfal1 Observation Sys圃.

  hl this paper, the血ee−year observation results ofMETROS will be reported.

2.Observation Methods

  The automatic recording血ermometers(temperature and humidity logger No.3(舛1 made by

Hiold electrical machineτy Co., Ltd.)were installed into the instrtmient shelters of 100 elementa【y

schools舳abo耐2.5㎞s脚al resol面on血Tokyo 23 wardS in July 2002(METROS100).

The meteorological instrumentS for wind direction and velocity, air temperature, air humidity,

precipitation and atmospheric pressure were also established on the rooftop of 20わuildings in 23

wards. The interval of these measurements was set up at 10 minutes. Then the data were automatically transmitted to the MRIEP and TMU(METROS20). The details of the METROS

are reported by Andoθ如1.(2003). In order to recognize the spatial stUcture of temperatUre, some contour maps were drawn by using these datasetS.

3.Resu】[ts and DiScussion

Spatia1 diS血喧butions of mean da鯛y maximum temperature in summer fbr three years

The s幽面面butions of me舳ily maximum temperature in summer for伽e years are

shown in Fig.1. Though the values of air temperature alre obviously different in each year, the spatial structures are similar among three years. The region with high temperature extends丘om the central Tokyo district toward the northem and northwestem parts of wards area. On the other

han¢10w air temperatures appear along the Tokyo Bay shore region exceμfbr Minato Ward,

especially, remarkably low in Edogawa ward.

<2002> <2003> <2004>

Fig.1 Spatial distributions ofmean(ぬily m砥㎞㎜血t㎝p㎝血e(°C)血summer(丘om July 20 to

     S叩t㎝b砿30血eacねyear).

  The nomhern and nonhwestern wardS, where are expected to be cooled by the sea br㏄ze fbm

Tokyo Bay in the daytime, experience significantly high temperature. This suggests that these

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areas are heated by the wind through the central Tbkyo district, or the cooling effect of sea br㏄ze is very low」n addition, the ascending current ofheat island circUlation in th6 central Tbkyo district

is considered to prevent the sea breeze丘om entering into the i血1and(Japan Meteorological

Agency 2006). On the other hand, it seems to become low temperature by the cool sea breeze in the coastal region ofTokyo Bay.

Spa伽1 d酌唖bu ons of mean da鯉y mh盛mum temperatUre in summer for the three years The s脚a1出s伽ions of mean daily minimum tem脚e in summer for血e血ee y…

shown in Fig.2. As well as the case of maximum temperatUre, the absolute values of temperatUre in each year are different. However, the spadal stmctures are similar among three years. The region with a relatively high temperature expands in the Tokyo Bay shore region including the central Tokyo district. There are clear and closed isothemlal lines around廿1e central Tokyo, and this result{s consistent with that of the past research, which showed that thc hcat island phenomena appeared clearly in the minimum tempera㈱dis面b砿ion肋l i舳e ma爵(im㎜

temperatUre distribution(Itoε o乙1994;Mikami 2003).

鷲一.

<2002> <2003> <2004>

晦2S酬is血bution ofme舳ly血㎞㎜雄te蝉血e(°C)㎞s−(丘om July 20 to

    September 30 in each year).

Spa髄al dis血董butions of proportion of hours above 300C

  Though there are many indices for expressing the high temperature in the daytine, such as a daily mar(imum temperature, tropical(ねy((iaily maximum temperatUre exceed血g 30°C), etc.,

these do not always indicate the impact of heat on our health. Ono(2004)demonstrated that the c翻er n㎜ber of he翫s面ke画e耐即idly血creased above 30°C i曲e(ia卿e. Therefore,面s temperature is considered to be good indicator and the total hours above 30°C seem to well express the血fluence on health in the daydme. The spatial disnibutions of proportion of hours above 30°C are sho㎜in Fig.3. The region With high propOnion tendS to extend丘om the central

Tokyo district to the northern and nonhwestern wardS. However it exp舳㎞血a e器t m血er血an

the corresponding area with relatively high tempera加re in Fig.1二It is necessary to pay more attention to the heat stroke in these regions than inσther region.

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<2002> <2003>

蟹讃 

饗搬欝

<2004>

  熱  ASt

撚鐸野

Hg.3 Spatial distributions ofproportion ofhours above 30°C(%)to all time血s−

    (from July 20 to Septeniber 30)

The spa髄al distribu髄on of the days of ton通d night

  The tonid night(daily minimum temperatUre exceeding 25°C)is related not only wi止止e

sleeplessness but also v舳血e heat stroke(Ministry of血e E曲onment 2005). Figure 4 shows血e

s蜘ldis轍ions of血e number of tonid nights iri summer for止e血ee yeπs. The regions wi出

a 1arge number of torrid night days exist in central Tokyo district and Tokyo Bay shore regions except for Edogawa and Koto wardS. The number of tonid night days seems to be relatively few

㎞the northwest area.

<2002> <2003> <2004>

Fig.4 Sp翻dis伽ions ofto㎡d蛸d細s㎜er(丘om July 20 to September 30).

4.Condusions

  As a result of high−density meteorological observadon by METROS, the actual condition of heat island phenomena in 23 wards was illustrated in detail. The main results are as f〈)110ws.

(1)For(laily maximum temperatUre,止e region with relatively high temperature extends fro舳e

  cent【al Tokyo district to the nonhern and nonhwestern wardS.

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(2)Relatively high tempera加re血daily minimum temperature was distributed over血e Tokyo

   Bay shore including 1血e centra1 Tokyo dis廿ict.

(3)The spatial disUibution of number of hours above 30°C is comparatively similar to that of

   daily maximum temperature. However, the region with止e high proportion of hours abOve

   30°Cwas l甑ed舳er eおt in com脚son舳血e warmer area as to(laily maximum

  temperature.

(4)Since the central Tokyo district has sign茸ica皿1y high temperatures both in the daytime and in   the nightthne, and also raises the tempera加re in the a(lj acent north and northeast area, it is   necessary to take countermeasures preferentially to this distdct.

References

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   Report ofthe Todソo Met.・Res. Inst.ノわr En・v. Protectio〃2003:81−87.**

Ito, M., Udagawa, M., and Mikami, T.1994. StUdy on the distribution ofthe temperature in Tokyo.

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Mikami, T., Wakabayashi, M., Udagawa, M., and lto, M.1997a. Urban heat island phenomena in

   Tokyo:Part l.−Repro(lucibility simulation of present conditions by numerical model−.

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Mikami, T., Wakabayashi, M., Udagaw璃 M.,{md Ito, M.1997b. Ufb{m heat island phenomena in    Tokyo:Part2.−Measures for reducing heat island intensity and their effectS−.肋〃ua〃leport    qプthe Tokソo。ルfet Res. Inst.ノbr Env Protection 1997:49−56.**

Mika ni, T.2003. Actual condition of urban heat islandS in Japan. Environ〃2ε吻1㈱肋碗oη    Science 32:32−36.**

Mikami, T., Ando, H., Yokoyama, H., Yamaguchi, T., Ishii, K., Shi(血, T., Modshi鵬W.,

Koj ima S。,㎝d㎞i, T.2004. Spatiotempora1 variation of summer urben heat islandS in

   Tokyo.ノlnnua1 Report of〃le Todソo、Met. Rθ∫.1加孟ノわr En・v.1〕 ro彪ction 2004:11−17.*

Ministry of止e Environment 2005. Heisei−1 6nendo 1伽磁ηゐGε励o塒o剛血吻o〃助o〃

   nikαnsuru Chousa・Kent()u(3ンo〃iU 1丑)kOkUsho(2004 Research and Exa〃3 ηα〃oη伽彪〃lent of

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   htq):〃www.nies.gojp/hnpacガ,2007/10/31.*

Yokoya鵬H., Ando, H., Yamaguchi, T., Ichino, M., Akiyama, Y., Ishii, K., and Mikami T.2005.

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(*:in Japanese,**:in Japanese with English abstract)

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