Communicating potentially large but non‐robust changes in multi‐model projections of future climate. (19th February 2021)
- Record Type:
- Journal Article
- Title:
- Communicating potentially large but non‐robust changes in multi‐model projections of future climate. (19th February 2021)
- Main Title:
- Communicating potentially large but non‐robust changes in multi‐model projections of future climate
- Authors:
- Zappa, Giuseppe
Bevacqua, Emanuele
Shepherd, Theodore G. - Abstract:
- Abstract: The future climate projections in the IPCC reports are visually communicated via maps showing the mean response of climate models to alternative scenarios of socio‐economic development. The presence of large changes is highlighted by stippling the maps where the mean climate response (the signal) is large compared to internal variability (the noise) and the response is robust, that is, consistent in sign, across the individual models. In addition, hatching is used to mark the regions with a small multi‐model mean change. This approach may fail to recognize the risk of large changes in regions where the uncertainty is large and the response is not robust. Here, we present a more informative diagnostic to support risk assessment that is obtained by quantifying the mean forced signal‐to‐noise ratio of the individual model responses, rather than the signal‐to‐noise ratio of the mean response. This enables us to identify regions where a large future change compared to year‐to‐year variability is plausible, regardless of whether the signal is robust across the ensemble. For mean precipitation changes, we find that the majority (58% in surface area) of the unmarked regions and a sizeable portion (19%) of the hatched regions from the AR5 projections hid climate change responses to the RCP8.5 scenario that are on average large compared to the year‐to‐year variability. Based on the newer CMIP6 ensemble, a considerable potential for large annual‐mean precipitation changes,Abstract: The future climate projections in the IPCC reports are visually communicated via maps showing the mean response of climate models to alternative scenarios of socio‐economic development. The presence of large changes is highlighted by stippling the maps where the mean climate response (the signal) is large compared to internal variability (the noise) and the response is robust, that is, consistent in sign, across the individual models. In addition, hatching is used to mark the regions with a small multi‐model mean change. This approach may fail to recognize the risk of large changes in regions where the uncertainty is large and the response is not robust. Here, we present a more informative diagnostic to support risk assessment that is obtained by quantifying the mean forced signal‐to‐noise ratio of the individual model responses, rather than the signal‐to‐noise ratio of the mean response. This enables us to identify regions where a large future change compared to year‐to‐year variability is plausible, regardless of whether the signal is robust across the ensemble. For mean precipitation changes, we find that the majority (58% in surface area) of the unmarked regions and a sizeable portion (19%) of the hatched regions from the AR5 projections hid climate change responses to the RCP8.5 scenario that are on average large compared to the year‐to‐year variability. Based on the newer CMIP6 ensemble, a considerable potential for large annual‐mean precipitation changes, despite the lack of a robust multi‐model projection, exists over 22% of the surface land area, particularly in Central America, northern South America (including the Amazon), Central and West Africa (including parts of the Sahel), and the Maritime Continent. Abstract : In the communication of climate change to stakeholders and policymakers the focus has been placed on highlighting those regions where there is agreement in the models' projections of large future changes. Yet, for risk assessment, the potential for large future changes should also be recognized even if the models do not agree and there is larger uncertainty. We here introduce a new diagnostic to evaluate multi‐model projections and show that, if emissions are not reduced, future precipitation changes as large as the inter‐annual variations may potentially affect an additional 22% of global land surface area (open stippling), which is otherwise not identified with the traditional approach focused on model agreement (full stippling). … (more)
- Is Part Of:
- International journal of climatology. Volume 41:Number 6(2021)
- Journal:
- International journal of climatology
- Issue:
- Volume 41:Number 6(2021)
- Issue Display:
- Volume 41, Issue 6 (2021)
- Year:
- 2021
- Volume:
- 41
- Issue:
- 6
- Issue Sort Value:
- 2021-0041-0006-0000
- Page Start:
- 3657
- Page End:
- 3669
- Publication Date:
- 2021-02-19
- Subjects:
- climate change -- climate model -- CMIP5 -- CMIP6 -- IPCC -- precipitation -- signal‐to‐noise -- time of emergence
Climatology -- Periodicals
Climat -- Périodiques
Climatologie -- Périodiques
551.605 - Journal URLs:
- http://onlinelibrary.wiley.com/ ↗
- DOI:
- 10.1002/joc.7041 ↗
- Languages:
- English
- ISSNs:
- 0899-8418
- Deposit Type:
- Legaldeposit
- View Content:
- Available online (eLD content is only available in our Reading Rooms) ↗
- Physical Locations:
- British Library DSC - 4542.168000
British Library DSC - BLDSS-3PM
British Library STI - ELD Digital store - Ingest File:
- 24489.xml