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0744 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
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キャプション

[Figure] Table 2. ヤンギ・クルからクム・チャプガンまでのタリム川(西支流)。The Tarim river (western branch) from Jangi-köl to Kum-tschapghan.

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

OCR読み取り結果

 

592   THE HYPSOMETRICAL RALATIONS OF THE TARIM BASIN.

Table 2.

The Tarim river (western branch) from Jangi-köl to Kum-tschapghan.

Month and day

1900.

s. 1o3.

Length in kilometers along the river.

Difference of   Corrected

altitude in difference of

meters.   altitude iu.

meters.

Hydrometrical station.

Jangi-köl   

Kirtschin-tarim    

Still water    

Tarim    

Still water    

Tarim    

Tarim at Ajagh-arghan . Almontschuk-tarim . . Schirge-tschapghan . .

Tschigilik-uj    

Still water    

   May 16   0.233

  •  21   0.829
    0.0ô0

   0.225   88.5

   0.000   16.2

May 28

  •  30

June I

  •  4

  •  5

  •  10

s I2

   27.3   •   6.4   4.0

   47.5   39 4   24.7

   29.6   0 0   0.o

   19.9   12.5

   0.o   0.0

   48.35   8.7   5.5

   17.75   I.5   '   1.0

   54.65   1 3 3   8.3

   65.2   8.o   5.o

   28.25   1.8   I .1

8.i   0.0   0.o

0.173 0.082 0.243 0.I24 0.065 0.000

Jurt-tschapghan    

Ku m-tschapghan    

Total

1901

April 3 and 13 June 25

April 10

0.047   61.1

O 021   3 5   I

I   -   I 496 0   I

2.9   1.8

0.1

102.0   64.0

0.I

Thus according to the hydrometrical data Kara-koschun would be 102.o meters lower than Jangi-köl. But this is no doubt too much. For by means of 136 meteorological observations made by Dr. Hedin in the Tarim delta at Kara-koschun and its environs and of simultaneous observations made at the permanent stations Jangiköl and Tscharklik, the probable altitude of Kara-koschun above sea-level appears to be 816 meters. Now the altitude of Jangi-köl being 881 meters, and supposing Kum-tschapghan to be i meter above Kara-koschun, the difference of altitude between Jangi-köl and Kum-tschapghan ought to be 64 meters. For this reason

I have reduced all differences of altitude in the above table in the rate Iô4 and

thus found the corrected numbers given in the last column, which I consider as the most probable.

Now the length of the river was measured between all stations from Jangiköl to Kum-tschapghan and a curve drawn as explained above, with the lengths as abscissa and the altitudes above Kum-tschapghan as ordinates. and from this construction the following table was obtained.