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0742 Scientific Results of a Journey in Central Asia, 1899-1902 : vol.2
1899-1902年の中央アジア旅行における科学的成果 : vol.2
Scientific Results of a Journey in Central Asia, 1899-1902 : vol.2 / 742 ページ(カラー画像)

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doi: 10.20676/00000216
引用形式選択: Chicago | APA | Harvard | IEEE

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590   THE HYPSOMETRICAT RELATIONS OF THE TARIN BASIN.

Table 1 (ended).

Name o f station.   I

Sarik-buja    Nov. 16   40° 58' 83' 45' —   430.8   6o   941

Kitschik-hasanak . . .    » 17   4o 58 83 52    —   415 6   59   940

Tschong-aralning-toghrighi   » 18   40 55 84 4 I —   396 9   58   939

Koral-dung     1   » 19   40 55 84 5 0.055   395.8   58   939

~   I

Kakte    19   40 55 , 84 14 —   376.7   57   938

Kätschik    » 20   40 54 ; 84 24 '—   364.2   56   937

Kätschkin-aghis    > 21   40 48 84 32 —   337.0   54   935

Unnamed camp    » 22   40 42 84 46 —   310.8   50   931

Unnamed camp    » 23   40 46 84 56 —   z88.1   46   927

Sadik-bajning-angi .   » 24   40 46 j 84 57 0.164 '   284.0   46   927

Kargha-jakti    » 24   40 45 i 85 5   —   265.9   42   923

Tokus-kum    » 25   40 43 ; 85 17 —   239.2   39 ; 920

Al-katik-tscheke    » 26   4o 431 85 20' 0.117   232.3   38 ' 919

Busrugvar    » 27 ! 40 42 85 z8 —   207.1   35   916

Kum-tscheke (Siva) . .   » 28   40 45 ; 85 33 0.105   186.6   33   914

Kurugen-ugen     .   » 29 ' 40 49 85 39 —   164.1   31 ' 912

Ait-öttögön    » 3o   4o 51 85 52   —   139.8   29 ' 910

Unnamed camp    Dec. 1   40 55 ' 86 1   123.8   27 , 908

Ilek    s   2   41 2 86 II   —   97.0   22   903

Momuni-ottogho   »   3   4t 3 86 23 —   70.4   16   897

Karaul    ,   4   41 4 86 32 0.222   54.3   12   893

Teis-köl    =   6   40 57 86 42 —   24.7   5   886

Jangi-köl   ;   =   7   40 52 86 51 • —   o.o   0   881

Table I gives the result of the calculation of the part from Lajlik to Jangiköl. Its contents are fully explained by the headings. In the last column we find the altitudes of the stations above sea-level. Of these only that of Jangi-köl is determined directly from the barometriçal observations made at that station; all the other altitudes have been found by adding to the altitude of Jangi-köl the numbers of the last column but one. Now it is important to get some control over this result. For this purpose I have used the meteorological observations taken during the months September, October and November, and in the following way. The barometric observations during September were reduced to the altitude of Lajlik by means of the differences of altitude given in table I; the barometric observations during October were in a similar manner reduced to the altitude of Haradigan-kötek, and the barometric observations during November to the altitude of Modschi-toghrak, and the average pressure calculated for each month. Also the mean temperature of the air was calculated and the average pressure at the altitude of 80o meters above sea-level was taken from the isobaric maps for these months.

s. IO.3

Month 899d day Lat. N.

Long. E. from Greenwich.

Distance along the river from Jangi-köl in kilometers.

Altitude above Jangiköl in meters.

Altitude above sea-level in meters.