In this paper the variation of weather situation on the singularity accompanied with increase or decrease of annual mean sun-spot numbers is discussed. For this investigation, Lettaus concept of “specific singularity” is applied. We have found that the variation of weather situation accompanied with sun-spot numbers before and after the singularities such as December 30th, February 5th and April 6th is almost similar on the respective cases. (Fig. 8) The principal characters obtained are as follows. (I) On the singularity as divided by sun-spot numbers into three cases a), b) and, c), a) When the annual mean value of sun-spot numbers is larger than 60, the daily preciptatatatiion amout over Japan is somewhat plentiful than the normal value (Fig. 4, B), and the positive anomaly of daily mean temperature is observed over the western Japan. (Fig. 5, B). b) When the sun-spot number is smaller than 15, the negative anomaly of daily precipitation amount is especially remarkable along the Japan Sea side. (Fig. 4, E) On the same calendar day, the anomaly of daily mean temperature is negative over the eastern Japan. (Fig. 5, E) Over Japan and her neighbourhood, the number of cyclone and anticyclone is remarkably small. (Fig. 6, E) c) When the sun-spot number is between 15 and 60, the daily mean temperature over Japan is colder than the normal temperature. (Fig. 4, I) It may be considerd that this distribution relates closely to anticyclones locating over Tohoku district. (Fig. 5, I) (II) On the day before or after the temperature singularity showing the maximum range of frequency distribution of daily mean temperature, the anomalies of precipitation and temperature are also examind as related to the magnitude of sun-spot numbers. a) When the sun-spot number is larger than 60, the negative anomaly of daily precipitation amount is observed over the southwestern Japan with its center near Shikoku district. (Figs. 4, (A, C)) The temperature anomaly is positive over almost the whole Japan which its center over the northern Japan. (Figs. 5, (A, C)) It is probable that above characters become distinct when the anticyclones appear over the eastern China or the East China Sea. (Figs. 6, (A, C)) b) When the sun-spot number is smaller than 15, the positive anomaly of daiy mean precipitation is observed along the southern coast of Japan. (Figs. 4, (D, F)) The distribution of temperature anomaly is not so distinct in spite of the positive anomaly over the western Japan. (Figs. 5, (D, F)) Above distributions are primarily explained by anticyclones over Japan. (Figs. 6, (D, F)) c) When the sun-spot number is between 15 and 60, the positive anomaly of precipitation is observed over the western Japan, (Figs. 4, (G. I)) and the temperature anomaly is negative over the area which extends from the west of Tohoku district through Shikoku district. (Figs. 5, (G, I)) It may be seen that these results are caused by numerous cyclones over the East China Sea. (Figs. 6, (G, I)) As already noted, variation of the distriburions of daily precipitator amount and daily mean temperature corresponding with that of the sun-spot numbers are caused indirectly by the passage of cyclones and anticyclones over Japan and her neighbourhood. This result is also verified by comparing the frequency distributions of daily mean temperature at Hiroshima. (Fig. 7)
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