Since the unusually hot summer in 1994, extremely high temperatures have frequently been observed in the midsummer season in Japan. As a possible factor increasing the heat, the urban heat island effect has received public interest, calling for political and technical measures to alleviate it. However, it still remains uncertain whether and how the urban effect contributes to the recent heat. The present paper aims to describe the spatial distribution and trends of high temperature with attention to urban anomalies using the data of the Automated Meteorological Data Acquisition System (AMeDAS) network.
The analysis of the spatial distribution of high temperature is based on daily maximum and minimum temperatures (
Tmax and
Tmin) defined from 10-minute data for the period 1994-2002. The daytime high temperature (
Tmax_??_35°C,
Tmax_??_38°C, and the annual extreme of
Tmax) was the most pronounced in the inland part of three large urban complexes centered on Tokyo, Osaka, and Nagoya. The nocturnal high temperature (
Tmin_??_25°C and T
min_??_28°C) was pronounced at coastal stations and in large cities, especially in Osaka and Tokyo. These features are apparently in agreement with previous studies on the urban heat island, which is characterized by nocturnal warming in the central area of cities and daytime warming on the inland side of large urban complexes located on the coast.
To evaluate the trend of high temperature in recent decades, the ten highest values of
Tmax and
Tmin in each year and their deviation from the 850-hPa temperature were analyzed using hourly data from 1979 to 2002. There were rising trends in
Tmax and
Tmin on the order of 1°C/(20 years) in a wide area from central Honshu to Kyushu. The change at 850 hPa accounts for only a fraction of these changes. These facts indicate rapid warming in the background field during the past few decades, with a larger amplitude in the boundary layer than in the free atmosphere. The signal of urban warming is nearly concealed in this change, but there are some anomalous trends of
Tmax in the inland areas adjacent to the three cities by 0.2-0.4°C/(20 years) in comparison with surrounding regions. This implies the existence of slowly intensifying urban warming, which can have a substantial impact on a time scale of several decades or a hundred years.
In conclusion, the frequent occurrence of extremely high temperature in the major urban areas in Japan can be attributed to the rapid background warming in the past few decades superimposed on the preexisting and slowly intensifying urban heat island.
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