the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Bioclimatic change as a function of global warming from CMIP6 climate projections
- 1College of Engineering, Mathematics and Physical Sciences, University of Exeter, Exeter, EX4 4QF, UK
- 2Global Systems Institute, University of Exeter, Exeter, EX4 4QE, UK
- 1College of Engineering, Mathematics and Physical Sciences, University of Exeter, Exeter, EX4 4QF, UK
- 2Global Systems Institute, University of Exeter, Exeter, EX4 4QE, UK
Abstract. Climate change is predicted to lead to major changes in terrestrial ecosystems (Pörtner et al., 2022). However, significant differences in climate model projections for given scenarios of greenhouse gas emissions (Masson-Delmotte et al., 2021), continue to hinder detailed assessment. Here we show, using a traditional Köppen-Geiger bioclimate classification system (Köppen, 1884), that the latest CMIP6 Earth System Models actually agree very well on the fraction of the global land-surface that will undergo a significant change per degree of global warming. Data from ‘historical’ and ‘ssp585’ model runs are used to create bioclimate maps at various degrees of global warming, and to investigate the performance of the ensemble mean when classifying climate data into discrete categories. Using a streamlined Köppen-Geiger scheme with 13 classifications, global bioclimate classification maps at 2 K and 4 K of global warming above a 1901–1931 reference period are presented. These projections show large shifts in bioclimate distribution, with an almost exclusive change from colder, wetter bioclimates to hotter, dryer ones. Historical model run performance is assessed and examined by comparison with the bioclimatic classifications derived from the observed climate over the same time period. The fraction (f ) of the land experiencing a change in its bioclimatic class as a function of global warming (∆T ) is estimated by combining the results from the individual models. Despite the discrete nature of the bioclimatic classification scheme, we find only a weakly-saturating dependence of this fraction on global warming f = 1 − e −0.17∆T , which implies about 12 % of land experiencing a significant change in climate, per 1 K increase in global mean temperature between the global warming levels of 1 and 3 K. Therefore, we estimate that stabilising the climate at 1.5 K rather than 2 K of global warming, would save over 7 million square kilometres of land from a major bioclimatic change.
Morgan Sparey et al.
Status: final response (author comments only)
-
RC1: 'Comment on bg-2022-74', Anonymous Referee #1, 22 Apr 2022
The authors present an analysis of Köppen-Geiger climate classification for several different levels of global warming using CMIP6 runs from six GCMs and investigate how the land area covered by different climate types changes as the degree of warming increases. The novelty of this work is the use of CMIP6 runs and the focus on degree of warming rather than a particular future point in time. The development of an equation to estimate the % land area that changes climate type as temperature increases is a nice simple metric for communicating projected changes in climate type and associated bioclimatic impacts.
One potential additional improvement to the manuscript would be to develop equations, like that in Equation 1 for the % land area changing climate type, for each streamlined classification climate type of Table 2. As warming increases from 0K to 4K some of the streamlined climate types will increase in % land area covered and others will decrease. An equation for each streamlined climate type could be very interesting / useful as some climate types will expand and reduce at different rates compared to the global land area change in Equation 1. Adding an extra column to Table 2 with the equation for each climate type would be very useful additional information. This would allow researchers interested in particular bioclimates to use these results for their research.
The work presented is well written, interesting to a wide audience and is very appropriate for this journal. I highlight some comments below that should be addressed.
Specific comments
Line 53: change “data to to” to “data to”.
Table 1: while the following differences from Peel et al (2007) are largely minor and most likely do not impact the end results significantly, it is important to note them. The Ds climate correction is likely to be the most important and should be corrected.
- Criteria for C climate: change from “0ËC ≤ Tmin <18ËC, Tmax ≥ 10ËC” to “0ËC < Tmin <18ËC, Tmax ≥ 10ËC”.
- Criteria for Cs climate: change from “Pwwet ≥ 3*Psdry, Psdry < 4” to “Pwwet > 3*Psdry, Psdry < 4”.
- Criteria for D climate: change from “Tmin < 0ËC, Tmax ≥ 10ËC” to “Tmin ≤ 0ËC, Tmax ≥ 10ËC”.
- Criteria for Dw climate: change from “Pswet ≥ 10*Pwdry” to “Pswet > 10*Pwdry”.
- Criteria for Ds climate: change from “3*Psdry < Pwwet” to “3*Psdry < Pwwet, Psdry < 4”.
- Criteria for ET climate: change from “0ËC ≤ Tmax <10ËC” to “0ËC < Tmax <10ËC”.
Line 63: change “First, C and D climates follow a 0ËC threshold instead of 3ËC” to “First, C and D climates follow a 0ËC threshold instead of -3ËC”.
Line 75: I know data can now be considered as singular or plural, but I recommend changing “model and observational data is smoothed” to “model and observational data are smoothed”.
Line 85: what do you mean by “anomaly corrected fields”? Not all readers will understand this term or what it means, so more explanation is required.
Table 2: In Table 1 all second letters were capital (for example CFa rather than Cfa). However, in Table 2 a mixture of second letter capitalisation is used (see Subtropical). Please be consistent.
Figure 3: It would be better to increase the size of these four maps as it is very hard to see the differences when the maps are so small. Rather than one column of four maps, try two columns of two maps. Also, why are these KG maps called anomaly plots?
Figure 5a & 5b: the right column of numbers next to the colour bar is labelled “% Land-area 4K” in both 5a and 5b. I think this should be “% Land-area 1.5K” for 5a and “% Land-area 2K” for 5b.
Line 142: You refer to Figure 5a, but don’t you mean Figure 5c? Figure 5a shows the 1.5K results, whereas Figure 5c shows the 4K results. Hence the comment about Arctic Tundra should be updated to 75% less land-area.
Equation 1: you provide an equation, but no measure of how well this model fits the data. I realise there are only nine data points supporting this model fit, but a metric like R2 would be useful to indicate how well the model fits the data.
-
RC2: 'Comment on bg-2022-74', Anonymous Referee #2, 13 May 2022
In this study Sparey et al. analyse model output from six state-of-the-art earth system models to estimate the changes in land bioclimate classes under different degrees of global warming. First they find the multi-model ensemble mean of historical runs compares favourably with observations-based bioclimate changes, and second they use scenario-based model runs to estimate potential future bioclimate changes. They are able to summarise their findings with a single equation that shows model agreement and is useful to communicate potential consequences of global warming. The study uses a modelling approach that fits within the scope of BG. The manuscript has a clear motivation and is well outlined. However, I think it could be improved by addressing the following specific comments. Additionally, I list some technical details that could be corrected.
Specific comments
- I think the most critical point the authors should address is the lack of a scientific "discussion". There is no single reference to other works in Section 3. For instance, how do these results compare with Kim and Bae (2021)? Are these results far away from similar works with CMIP5 like Rahimi et al. (2020)? Here I only refer to those citations in the Introduction, but perhaps there exists more literature that can be discussed. Keeping together "Results and Discussion" is possible, but in this case I think Section 3 only includes a description of the outcome of the author's own analyses.
- Also, besides using references for the discussion section, I think the authors should revise the use of references throughout the manuscript. For instance in the Introduction there are no references about CMIP6 or the Paris climate targets. Also when the authors say in line 60 that the scheme has had many alterations, they could provide a list of some publications in parentheses with as e.g..
- Is Table 1 and the modifications described in lines 62-65 the same as in Peel et al. (2007)? Or are these the author's own modifications to what Peel et al. (2007) do? Please also consider including a citation in the caption of Table 1 if this is indeed taken from the reference.
- Authors should motivate better their model selection process. This is especially important since the 6 chosen models include repeated model components. How different are, for instance, CanESM5 and CanESM5-CanOE in terms of simulated (atmospheric variables) monthly precipitation and temperature values?What are the "data management" reasons that lead to these 6 models being selected over other models?
- Along with the previous comment, please include a table with the specifications of the data used. Since the model output data is a critical component of this study, it is important that some characteristics (e.g., spatial resolution, time step, citation to techanical paper) can be readily seen and compared in a table.
- Please discuss possible shortcomings of downscaling model output to a finer grid (0.5°), in case this was done when the model output is at a coarser scale. This is why a table with some specifications of the data could be useful.
- Please consider providing maps like those in Appendix A but using the "streamlined" version.
- In multiple occasions the word "significant" is used. I think that with the data the authors have it should be possible to perform some statistical significance tests. I think such tests could increase the strength of the results. Without the tests, please consider alternating with synonyms like "substantial", "marked", "large" or alike.
Technical details
- Please consider re-organising some paragraphs in the Introduction. Paragraph starting on line 35 may fit better after the description of the classification systems. As a side note, this paragraph does not mention any references about CMIP6.
- I would recommend to move the sentence about previous applications of KG (line 43) to the end of Section 2.1.
- Abstract contains references. Are they urgently required?
- Consider prefixing "ensemble mean" with "multimodel", because some times "ensemble" could be referring to a group of runs or data.
- Please include spaces between numbers and their units, and use units in exponential notation (e.g., cm month-1)
- I think authors should mention vegetation in some places. At least when explaining the KG classification system on line 32.
- Perhaps Section 2.4.1 should actually be a subsection of or follow the Section on the traditional KG scheme (Section 2.1).
- Please expand on what the anomaly corrections are.
- Consider using "averaging" instead of "meaning".
In the following I refer to specific lines (L):
- L3: "hinder" -> maybe "limit" is an alternative. Many detailed assessments can be made in spite of inter-model spread.
- L4: why capitalisation in "Earth System Models".
- L4: remove "very".
- L5: "will" -> "would".
- L21: Is it correct "regional areas"?
- L31: missing umlaut in Köppen name.
- L43: maybe this "most popular" should be referenced. Otherwise "popular" should suffice.
- L50: review "more intuitive".
- L52: review this sentence.
- L60: check citation is \textcite, not \parencite.
- L72: please use active voice: "we do not expect".
- L76: check if "correctly" can be replaced by "following observations".
- L80: is it above pre-industrial levels or above the reference period 1901--1931?
- L81: remove "model" after "CMIP6".
- L90: review this sentence.
- L110: remove period after "Figure 1".
- L116: (and Fig. 1 and 2 captions) consider "averaging process" instead of "meaning".
- L117: 'lagging' as in having lower values?
- L119, L120: check use of "correctly", that can always be related to "according to observation-based KG".
- L129: check "real world climate".
- L134: use cross-referencing with the appendices (e.g., Appendix A).
- L135: "shows" -> "suggests". "will be" -> "could be".
- Fig. 3 caption: maybe place "reference period" before CMIP6 ssp585 runs.
- L162: "will" -> "could".
Morgan Sparey et al.
Morgan Sparey et al.
Viewed
| HTML | XML | Total | BibTeX | EndNote | |
|---|---|---|---|---|---|
| 297 | 65 | 12 | 374 | 6 | 5 |
- HTML: 297
- PDF: 65
- XML: 12
- Total: 374
- BibTeX: 6
- EndNote: 5
Viewed (geographical distribution)
| Country | # | Views | % |
|---|
| Total: | 0 |
| HTML: | 0 |
| PDF: | 0 |
| XML: | 0 |
- 1