表(Table)
* 表题
- Table 2.10. Mean temperature differences between the Brochen (1134 m) and the free atmosphere at Wengerode. April 1957—March 1962. 表2.10. 1957 年4 月到1962 年3 月在Brochen (1134 米)测点和Wengerode 自由大气中(月)平均气温差.
GMT*
J
F
M
A
…
D
YR AV.
00
12
(After Hansel, 1962) (引自Hansel,1962)
*local time is one hour ahead of GMT. *当地时间比格林尼治平时早1 小时.
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Table 1. Correlation coefficients between various SASM indices.
SASMI WYI MHI AIRI SASMI1 SASMI2
SASMI 1.00 0.72 0.58 0.68 0.88 0.63
WYI 1.00 0.49 0.49 0.65 0.46
MHI 1.00 0.63 0.61 0.08
AIRI 1.00 0.73 0.08
SASMI1 1.00 0.26
SASMI2 1.00
Calculations are based on seasonal means on June–September 1958–98. Coefficients that are significant at the 99.9% confidence level are bolded. SASMI, SASMI1 and SASMI2, see text. WYI [Webster and Yang, 1992], the zonal wind shear between 850hPa and 200hPa averaged over the area (0°– 20°N, 40°–110°E). MHI [Goswami et al., 1999], the meridional wind shear between 850 hPa and 200 hPa average over the region (10°–30°N, 70°–110°E). AIRI [Shukla and Paolino, 1983; Parthasarathy et al., 1994], the seasonally average precipitation over the Indian subcontinent from June to September.
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* 分析
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Table 1 shows (lists, gives, presents, indicates, summarizes, outlines, tabulates, illustrates, is a summary of) results from a June 1982 Zodiac rubber boat sampling experiment in ring center 82-B. The boat samples (the first four rows of data) were collected from a depth of 0—5m.
表1给出1982年6月在82-B圆形海域中心乘橡皮船Zodiac号取样试验的资料。该船采集的样本(前4 行资料)取自0—5 米深度。
- The value of R by (18) may be in error by as much as 20%, as shown (listed, given, presented) in the table. 如表所示,用方程(18)求出的R 值其误差可能会高达20%。