2004
DOI: 10.1023/b:clim.0000043136.58100.ce
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Urbanization Effect on the Observed Change in Mean Monthly Temperatures between 1951–1980 and 1971–2000 in Korea

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Cited by 90 publications
(53 citation statements)
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“…The overall population density in Doha is approximately 3000 persons/ km 2 , with the maximum value within the city of greater than 10,000 persons/km 2 . DIA is nowadays located in a highly urbanized area, and urbanization is one of the primary causes of an intensified heat island effect, and an increase in population has been shown to correlate with terrain warming in urban areas (Chung et al 2004). Published literature has noted that urban warming is more pronounced during summer evenings (Karl et al 1993) because urban structures release heat that has been absorbed during the day.…”
Section: Discussionmentioning
confidence: 99%
“…The overall population density in Doha is approximately 3000 persons/ km 2 , with the maximum value within the city of greater than 10,000 persons/km 2 . DIA is nowadays located in a highly urbanized area, and urbanization is one of the primary causes of an intensified heat island effect, and an increase in population has been shown to correlate with terrain warming in urban areas (Chung et al 2004). Published literature has noted that urban warming is more pronounced during summer evenings (Karl et al 1993) because urban structures release heat that has been absorbed during the day.…”
Section: Discussionmentioning
confidence: 99%
“…Urbanization effects were found to be common in all months except April, and up to 0.5°C of the reported increases in Korean night-time temperature were induced by urbanization (and not regional warming) in the later normal period compared with the earlier normal period. In contrast, it was estimated that the urbanization effect on daily maximum temperature change was small (Chung et al, 2004).…”
Section: Climate Station Selection and Urbanization Issuesmentioning
confidence: 96%
“…The maximum UHI in Seoul has increased by an estimated 0.56°C over the period 1973-96 (Kim andBaik, 2002), whereas the estimated average annual urban bias in South Korea mean temperatures over the 1968-99 period was ∼0.4°C (Choi et al, 2003). Determination of urbanization effects versus regional climate-change effects in apparent (recorded) temperature change in Korea was undertaken (Chung et al, 2004), using two normal periods (1951-80 versus 1971-2000), and utilizing population data. Urbanization effects were found to be common in all months except April, and up to 0.5°C of the reported increases in Korean night-time temperature were induced by urbanization (and not regional warming) in the later normal period compared with the earlier normal period.…”
Section: Climate Station Selection and Urbanization Issuesmentioning
confidence: 99%
“…반면 일 평균운량이 9 이상인 흐린 날(33일)의 기온감률은 ME -0.0006℃/m로 대체로 실측치가 추정치 보다 더 작았다. 흐린 날은 401m와 313m 두 지점간 기온 편차(=실측 기온감률)가 하루 동안 거의 일정하게 (Chung et al, 2004;2006;2009;Kim et al, 2010;2012Kim and Yun, 2011;2014) …”
Section: 이를 기온 표준곡선의 동일 시간대 기온편차와 대응시unclassified