The Carbon Dioxide Removal Model Intercomparison Project (CDRMIP): rationale and experimental protocol for CMIP6

• الحاوية / القاعدة: Geoscientific Model Development
• المؤلفون الرئيسيون: D. P. Keller, A. Lenton, V. Scott, N. E. Vaughan, N. Bauer, D. Ji, C. D. Jones, B. Kravitz, H. Muri, K. Zickfeld
• التنسيق: مقال
• اللغة: الإنجليزية
• منشور في: Copernicus Publications 2018-03-01
• الموضوعات: open climate campaign
• الوصول للمادة أونلاين: https://www.geosci-model-dev.net/11/1133/2018/gmd-11-1133-2018.pdf

The recent IPCC reports state that continued anthropogenic greenhouse gas emissions are changing the climate, threatening <q>severe, pervasive and irreversible</q> impacts. Slow progress in emissions reduction to mitigate climate change is resulting in increased attention to what is called geoengineering, climate engineering, or climate intervention – deliberate interventions to counter climate change that seek to either modify the Earth's radiation budget or remove greenhouse gases such as CO₂ from the atmosphere. When focused on CO₂, the latter of these categories is called carbon dioxide removal (CDR). Future emission scenarios that stay well below 2 °C, and all emission scenarios that do not exceed 1.5 °C warming by the year 2100, require some form of CDR. At present, there is little consensus on the climate impacts and atmospheric CO₂ reduction efficacy of the different types of proposed CDR. To address this need, the Carbon Dioxide Removal Model Intercomparison Project (or CDRMIP) was initiated. This project brings together models of the Earth system in a common framework to explore the potential, impacts, and challenges of CDR. Here, we describe the first set of CDRMIP experiments, which are formally part of the 6th Coupled Model Intercomparison Project (CMIP6). These experiments are designed to address questions concerning CDR-induced climate <q>reversibility</q>, the response of the Earth system to direct atmospheric CO₂ removal (direct air capture and storage), and the CDR potential and impacts of afforestation and reforestation, as well as ocean alkalinization.>