Japan Geoscience Union Meeting 2023

Presentation information

[E] Online Poster

A (Atmospheric and Hydrospheric Sciences ) » A-CG Complex & General

[A-CG34] Projection and detection of global environmental change

Wed. May 24, 2023 9:00 AM - 10:30 AM Online Poster Zoom Room (3) (Online Poster)

convener:Michio Kawamiya(Japan Agency for Marine-Earth Science and Technology), Kaoru Tachiiri(Japan Agency for Marine-Earth Science and Technology), Hiroaki Tatebe(Japan Agency for Marine-Earth Science and Technology), V Ramaswamy(NOAA GFDL)

On-site poster schedule(2023/5/23 17:15-18:45)

9:00 AM - 10:30 AM

[ACG34-P08] Identifying crucial emission sources under low forcing scenarios by a comprehensive attribution analysis

*Xuanming Su1, Kaoru Tachiiri2,1, Katsumasa Tanaka3,1, Michio Watanabe2, Michio Kawamiya2 (1.National Institute for Environmental Studies, Japan, 2.Japan Agency for Marine-Earth Science and Technology, 3.Laboratoire des Sciences du Climat et de l'Environnement)

Clarifying the contributions of radiative forcings from different regions, sectors, and climate forcers can help policymakers understand the relative importance of various sources for meeting the Paris Agreement temperature targets. Here, we show a comprehensive study using a normalized marginal method to quantify such forcing contributions under scenarios toward the low forcing levels of 1.9 and 2.6 Wm−2 in 2100, proxies of the 1.5°C and 2°C targets of the Paris Agreement, respectively. We found that the distribution of forcing contributions appears to be similar between the present and 2100 by region, though it differs substantially by sector and climate forcer. Most developing regions and housing and transport sectors yield larger forcings in 2100 than at present under low forcing scenarios. Achieving low forcing levels strongly relies on negative CO2 emissions under the scenarios we considered. Finally, our results indicate a crucial role for China in reducing end-of-the-century forcing contributions from high to low levels.

Fig 1. Regional forcing contributions under the historical and two future scenarios with low forcing levels