朱福康. 1964: 多年月平均500毫巴图上60°N和30°N纬圈的波谱分析. 气象学报, (1): 31-40. DOI: 10.11676/qxxb1964.004
引用本文: 朱福康. 1964: 多年月平均500毫巴图上60°N和30°N纬圈的波谱分析. 气象学报, (1): 31-40. DOI: 10.11676/qxxb1964.004
CHU FU-KANG. 1964: POWER-SPECTRA ANALYSIS ON THE MEAN MONTHLY MAPS OF 500 MB LEVEL AT LATITUDES 60°N AND 30°N. Acta Meteorologica Sinica, (1): 31-40. DOI: 10.11676/qxxb1964.004
Citation: CHU FU-KANG. 1964: POWER-SPECTRA ANALYSIS ON THE MEAN MONTHLY MAPS OF 500 MB LEVEL AT LATITUDES 60°N AND 30°N. Acta Meteorologica Sinica, (1): 31-40. DOI: 10.11676/qxxb1964.004

多年月平均500毫巴图上60°N和30°N纬圈的波谱分析

POWER-SPECTRA ANALYSIS ON THE MEAN MONTHLY MAPS OF 500 MB LEVEL AT LATITUDES 60°N AND 30°N

  • 摘要: 本文对北半球多年月平均500毫巴图上60°N和30°N纬圈的高度和纬圈平均的经向运动动能进行了波谱分析,探讨了前3个波幅和位相角的季节变化,以及在高低纬度之间的差异。主要结果如下:1位势场的高度主要贡献,集中在准静止长波范围内,并具有明显的季节变化。2波数为1的波在高低纬度性质有显著的不同,其分界线大约在50°-60°N之间。此外,准静止的长波愈向低纬度去逐渐有向西偏移的现象。例如,在30°N上准静止的长波比60°N上要偏西(1/4)-(1/2)波长。360°N纬圈平均的经向运动动能主要部分亦集中在准静止长波范围内。虽然峰值有明显的季节变化,但最大的极值都出现在波数n=2-4之间。30°N纬圈平均的经向运动动能谱有着明显的季节变化,大致可分成如下3个类型:(1)冬季型:纬圈平均的经向运动动能谱存在着两个极值,最大的极值稳定于准静止长波范围内(n=3附近),次极植位于移动性行星波范围内(n=5-8)。(2)夏季型:纬圈平均的经向运动动能谱只有一个极值,稳定于波数为6-7的波内。(3)过渡型:纬圈平均的经向运动动能谱分布较平坦,没有稳定的极值存在。

     

    Abstract: Spectra analyses on the potential field and the zonally-averaged kinetic energy of meridional motions on the mean monthly 500 mb maps of Northern Hemisphere at latitudes of 60°N and 30°N have been made. The seasonal variations of the amplitudes and phase angles of the first three waves and the differences between high and low latitudes of these quantities, are studied in detail. The results are as follows:1) The chief contributions of the normal potential field are mainly concentrated at the long quasi-stationary waves and show significant seasonal variations. 2) The waves of wave number one have significant differences in the latitudes north or south of about 50°-60°N. The quasi-stationary long waves displace gradually to the west as they approach to the lower latitudes. For example, the quasi-stationary waves at 30°N have been deviated by 1/4 to 1/2 wave lengths to the west from that at 60°N. 3) The primary component of the tonally averaged meridional kinetic energy along 600N is also concentrated in the quasi-stationary waves. The maximum value appears in the waves of wave number n=2-4, the peak value having significant seasoaal varia- tions. The spectra of the tonally-averaged meridional kinetic energy along 30°N caa be roughly classified into three types according to their seasonal variations: a) Winter type: the tonally-averaged meridional kinetic energy along 30°N has the highest maximum value at the quasi-stationary waves near wave number three and the secondary maximum value at the travelling planetary waves (near n=5-8).b) Summer type: the zonally-averaged meridional kinetic energy along 30°N has only one maximum value at the wave of wave number 6-7. c) Transient type: the spectrum of the tonally-averaged meridional kinetic energy along 30°N is rather flat and has no a stationary peak value.

     

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