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NTIS 바로가기대기 = Atmosphere, v.25 no.1, 2015년, pp.85 - 97
허태경 (국립기상과학원) , 부경온 (국립기상과학원) , 심성보 (국립기상과학원) , 홍진규 (연세대학교 대기과학과) , 홍제우 (연세대학교 대기과학과)
This study is to investigate future changes in carbon cycle using the HadGEM2-Carbon Cycle simulations driven by
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핵심어 | 질문 | 논문에서 추출한 답변 |
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IPCC 5차 보고서에 따르면 산업혁명 이후 인간 활동에 의해 대기 중으로 인위적으로 배출되는 온실가스는 1750년부터 2011년까지 약 얼마로 보고되었는가? | 산업혁명 이후 인간 활동에 의해 대기 중으로 인위적으로 배출되는 온실가스는 꾸준히 증가하고 있다. IPCC 5차 보고서에 따르면 인간활동에 의한 CO2 배출량이 1750년부터 2011년 까지 약 555 85 GtC yr-1로 보고되었다(IPCC AR5., 2013). | |
기후 모형의 장점은 무엇인가? | 전 지구적 규모의 탄소 수지 평가를 하고 탄소-기후상호 작용의 다양한 측면을 알아보는데 기후 모형은매우 유용하다. 특히 모형을 이용하면 육상생태계와 해양 생지화학 과정, 대기와의 교환과 같은 광범위의 탄소 순환의 탄소량 추정이 가능하다는 장점이 있다(Ito et al., 2008). | |
대기 중 CO2 농도 증가를 억제하는 역할에는 무엇이 있는가? | 육상 및 해양 생태계는 광합성을 통하여 이산화탄소를 흡수하여, 대기 중 CO2 농도 증가를 억제하는 주요한 역할을 하고 있다. 미래 기후 변화에 미치는 탄소순환의 영향과 또한 탄소순환에서 대기 중에 배출된 탄소는 육상, 해양과의 교환과정을 통해 대기 중으로 축적되는데, 이러한 육상과 해양에서의 탄소 흡수량은 육상 생물권과 해양의 생태계가 기후 변화에 의해 영향을 받으므로 CO2 흡수능력 역시 변화됨을 주목해야 한다. |
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