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Michio Kawamiya

Dados Biográficos

ID7995504
NOMEMichio Kawamiya
PRENOMESMichio
SOBRENOMEKawamiya
ASSINATURAKAWAMIYA M
AFILIAÇÕESJapan Agency for Marine-Earth Science and Technology
ORCID0000-0001-7553-0522
VERIFICADOSim
TOTAL DE OBRAS7
TOTAL DE CITAÇÕES0
TOTAL COMO AUTOR7
TOTAL COMO EDITOR0
PRIMEIRO ANO DE PUBLICAÇÃO2006
ANO MAIS RECENTE DE PUBLICAÇÃO2026
ÍNDICE H0
  • The High Value of Climate Mitigation in Limiting Global Fish Biomass Losses to the year 23

    Keith B Rodgers, Daniele Bianchi et al.•ARTICLE•2026

    It is widely understood that future climate change will have large deleterious impacts on marine ecosystems. Large synthesis efforts conducted to date by FishMIP with higher trophic level (HTL) models have shown that under high emissions scenarios, future fish biomass losses of the order of 20% can be expected by 2100. However, the impact of anthropogenic climate change beyond 2100 remains largely unexplored, even though policy choices made now w…

  • Degrees of reversibility of ocean deoxygenation in an atmospheric carbon dioxide removal scenario

    Open Access•Estela A Monteiro, David P Keller et al.•ARTICLE•Environmental Research Letters•2025

    Over the last century, increasing atmospheric carbon dioxide (CO 2 ) concentrations, among other greenhouse gases, and resulting climate change have greatly impacted the ocean. Observed impacts include lower oxygen solubility and changes in ocean stratification, circulation and biological activity. To reduce the carbon burden in the atmosphere in the future and thereby mitigate anthropogenic climate change, carbon dioxide removal (CDR) techniques…

  • Identifying crucial emission sources under low forcing scenarios by a comprehensive attribution analysis

    Open Access•Xuanming Su, Kaoru Tachiiri et al.•ARTICLE•One Earth•2022

  • Increase of the transient climate response to cumulative carbon emissions with decreasing CO 2 concentration scenarios

    Open Access•Kaoru Tachiiri, Tomohiro Hajima et al.•ARTICLE•Environmental Research Letters•2019

    Near-constancy of the transient climate response to cumulative carbon emissions (TCRE) facilitates the development of future emission pathways compatible with temperature targets. However, most studies have explored TCRE under scenarios of temperature increase. We used an Earth system model (MIROC-ESM) to examine TCRE in scenarios with increasing and stable CO 2 concentrations, as well as overshoot pathways in which global mean temperatures peak …

  • Effect on the Earth system of realizing a 1.5 °C warming climate target after overshooting to the 2 °C level

    Open Access•Kaoru Tachiiri, Diego Silva Herran et al.•ARTICLE•Environmental Research Letters•2019

    An Earth system model (ESM) was used to investigate the effect of reaching the target of 1.5 °C warming (relative to preindustrial levels) after overshooting to the 2 °C level with respect to selected global environment indicators. Two scenarios were compared that diverged after reaching the 2 °C level: one stayed at the 2 °C level, and the other cooled to the 1.5 °C level. Unlike the internationally coordinated model intercomparison projects, th…

  • Increase of uncertainty in transient climate response to cumulative carbon emissions after stabilization of atmospheric CO 2 concentration

    Open Access•Kaoru Tachiiri, Tomohiro Hajima et al.•ARTICLE•Environmental Research Letters•2015

    We analyzed a dataset from an experiment of an earth system model of intermediate complexity, focusing on the change in transient climate response to cumulative carbon emissions (TCRE) after atmospheric CO _2 concentration was stabilized in the Representative Concentration Pathway (RCP) 4.5. We estimated the TCRE in 2005 at 0.3–2.4 K/TtC for an unconstrained case and 1.1–1.7 K/TtC when constrained with historical and present-day observational dat…

  • Climate–Carbon Cycle Feedback Analysis

    Pierre Friedlingstein, Peter M Cox et al.•ARTICLE•Journal of Climate•2006

    Eleven coupled climate–carbon cycle models used a common protocol to study the coupling between climate change and the carbon cycle. The models were forced by historical emissions and the Intergovernmental Panel on Climate Change (IPCC) Special Report on Emissions Scenarios (SRES) A2 anthropogenic emissions of CO2 for the 1850–2100 time period. For each model, two simulations were performed in order to isolate the impact of climate change on the …

Sem obras proeminentes nesta página.

  • Climate–Carbon Cycle Feedback Analysis

    Pierre Friedlingstein, Peter M Cox et al.•ARTICLE•Journal of Climate•2006

    Eleven coupled climate–carbon cycle models used a common protocol to study the coupling between climate change and the carbon cycle. The models were forced by historical emissions and the Intergovernmental Panel on Climate Change (IPCC) Special Report on Emissions Scenarios (SRES) A2 anthropogenic emissions of CO2 for the 1850–2100 time period. For each model, two simulations were performed in order to isolate the impact of climate change on the …

  • Increase of uncertainty in transient climate response to cumulative carbon emissions after stabilization of atmospheric CO 2 concentration

    Open Access•Kaoru Tachiiri, Tomohiro Hajima et al.•ARTICLE•Environmental Research Letters•2015

    We analyzed a dataset from an experiment of an earth system model of intermediate complexity, focusing on the change in transient climate response to cumulative carbon emissions (TCRE) after atmospheric CO _2 concentration was stabilized in the Representative Concentration Pathway (RCP) 4.5. We estimated the TCRE in 2005 at 0.3–2.4 K/TtC for an unconstrained case and 1.1–1.7 K/TtC when constrained with historical and present-day observational dat…

  • Increase of the transient climate response to cumulative carbon emissions with decreasing CO 2 concentration scenarios

    Open Access•Kaoru Tachiiri, Tomohiro Hajima et al.•ARTICLE•Environmental Research Letters•2019

    Near-constancy of the transient climate response to cumulative carbon emissions (TCRE) facilitates the development of future emission pathways compatible with temperature targets. However, most studies have explored TCRE under scenarios of temperature increase. We used an Earth system model (MIROC-ESM) to examine TCRE in scenarios with increasing and stable CO 2 concentrations, as well as overshoot pathways in which global mean temperatures peak …

  • Effect on the Earth system of realizing a 1.5 °C warming climate target after overshooting to the 2 °C level

    Open Access•Kaoru Tachiiri, Diego Silva Herran et al.•ARTICLE•Environmental Research Letters•2019

    An Earth system model (ESM) was used to investigate the effect of reaching the target of 1.5 °C warming (relative to preindustrial levels) after overshooting to the 2 °C level with respect to selected global environment indicators. Two scenarios were compared that diverged after reaching the 2 °C level: one stayed at the 2 °C level, and the other cooled to the 1.5 °C level. Unlike the internationally coordinated model intercomparison projects, th…

  • Identifying crucial emission sources under low forcing scenarios by a comprehensive attribution analysis

    Open Access•Xuanming Su, Kaoru Tachiiri et al.•ARTICLE•One Earth•2022

  • Degrees of reversibility of ocean deoxygenation in an atmospheric carbon dioxide removal scenario

    Open Access•Estela A Monteiro, David P Keller et al.•ARTICLE•Environmental Research Letters•2025

    Over the last century, increasing atmospheric carbon dioxide (CO 2 ) concentrations, among other greenhouse gases, and resulting climate change have greatly impacted the ocean. Observed impacts include lower oxygen solubility and changes in ocean stratification, circulation and biological activity. To reduce the carbon burden in the atmosphere in the future and thereby mitigate anthropogenic climate change, carbon dioxide removal (CDR) techniques…

  • The High Value of Climate Mitigation in Limiting Global Fish Biomass Losses to the year 23

    Keith B Rodgers, Daniele Bianchi et al.•ARTICLE•2026

    It is widely understood that future climate change will have large deleterious impacts on marine ecosystems. Large synthesis efforts conducted to date by FishMIP with higher trophic level (HTL) models have shown that under high emissions scenarios, future fish biomass losses of the order of 20% can be expected by 2100. However, the impact of anthropogenic climate change beyond 2100 remains largely unexplored, even though policy choices made now w…

Climatology (6 obras) · Environmental Science (6 obras) · Atmospheric sciences (5 obras) · Climate change (5 obras) · Climate model (5 obras) · Geology (5 obras) · Atmospheric and Environmental Gas Dynamics (4 obras) · Carbon cycle (3 obras) · Carbon dioxide (3 obras) · Chemistry (3 obras)

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