An Increasing Trend in the Early Winter Precipitation during Recent Decades along the Coastal Areas of the Sea of Japan

2017 ◽  
Vol 18 (11) ◽  
pp. 2893-2906 ◽  
Author(s):  
Kazuaki Yasunaga ◽  
Masashi Tomochika

Abstract Long-term changes in the monthly precipitation along the coastal areas of the Sea of Japan are examined using monthly operational observation data from the Japan Meteorological Agency. The monthly precipitation in December significantly increased from the mid-1980s to 2015, even though no remarkable changes were found in January, February, or November. Significant positive trends in the December precipitation extend widely over the coastal areas of the Sea of Japan, and the amounts increase to approximately 50% of the climatological precipitation in December at most observational stations. The interannual variations in other variables, including the monthly accumulated actual sunshine duration, days with lightning detection, and satellite-retrieved outgoing longwave radiation, also show significant trends that are consistent with the precipitation increase in December. The effect of the sea surface temperature (SST) on precipitation change is discussed based on correlation and regression analyses. The interannual variations in the December precipitation averaged over the observational stations near the Sea of Japan are significantly correlated with the SSTs in the prior month (November). However, the SST increase in November is insufficient to account for the increase in precipitation. In addition, it was found that the satellite-retrieved surface wind speed in December has grown stronger in recent years over the Sea of Japan. It is suggested that the stronger wind corresponds to the enhanced monsoonal flow and is the primary cause of the precipitation increase in December.

2007 ◽  
Vol 73 (5) ◽  
pp. 880-890 ◽  
Author(s):  
KOUSUKE YATSUYA ◽  
TOMOKAZU NISHIGAKI ◽  
AKIO DOUKE ◽  
MASASHI ITANI ◽  
YOZO WADA

SOLA ◽  
2019 ◽  
Vol 15 (0) ◽  
pp. 234-237
Author(s):  
Kenichi Kusunoki ◽  
Ken-ichiro Arai ◽  
Hanako Y. Inoue ◽  
Chusei Fujiwara

2015 ◽  
Vol 143 (1) ◽  
pp. 54-63 ◽  
Author(s):  
Yuta Ando ◽  
Masayo Ogi ◽  
Yoshihiro Tachibana

Abstract Negative Arctic Oscillation (AO) and western Pacific (WP) indices persisted from October to December 2012 in the Northern Hemisphere. For the first time, the monthly AO and WP were both negative for three consecutive months since records have been kept. Although in general negative AO and WP phases cause Siberia, East Asia, and Japan to be abnormally cold, Japan was relatively warm in October 2012 even though both the AO and WP were strongly negative. The temperature of the Sea of Japan reached a record-breaking high in October 2012, and it was found that heating by these very warm waters, despite the small size of the Sea of Japan, overwhelmed the cooling effect of the strongly negative AO and WP in October. Linear regression analyses showed that Japan tends to be warm in years when the Sea of Japan is warm. Consequently, the temperature over Japan is controlled by interannual variations of small-scale oceanic phenomena as well as by large-scale atmospheric patterns. Previous studies have ignored such small-scale oceanic influences on island temperatures.


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