国立情報学研究所 - ディジタル・シルクロード・プロジェクト
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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 |
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.
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