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====== NEW PMIP publications for AR6 ====== | ====== NEW PMIP publications for AR6 ====== | ||
- | Document generated on **Wed Aug 28 15:11:35 2019** | + | Document generated on **Wed Sep 4 11:04:29 2019** |
Number of submitted references: **16** | Number of submitted references: **16** | ||
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* There may be some duplicates (same ref submitted by different people) | * There may be some duplicates (same ref submitted by different people) | ||
- | ===== Chapter 1: Framing, context, methods | + | ===== References |
- | + | ||
- | Number of selected references: **5** | + | |
- | + | ||
- | * Dmitry Yumashev* & Chris Brierley, The economic implications of using the true preindustrial climate baseline | + | |
- | * **Submitted** = //No// | + | |
- | * **Keywords** = //early industrial vs preindustrial// | + | |
- | * **Details** = This paper will look at the cost-benefit analysis of using a preindustrial or early-industrial baseline. Whilst these may be statistically equivalent, which one is picked could still cause differences between different economic blocs. | + | |
- | * **Why** = This wil be relevant for the cross-chapter box on preindustrial definitions. It's analysis demonstrates that even a choice as scientifically arbitrary as this has social justice implications. It also states that this difference only matters if the Paris Agreement is met, and so shouldn' | + | |
- | + | ||
- | * Charles J.R. Williams*, Maria V. Guarino, Joy S. Singarayer, Louise Sime, Emilie Capron, Daniel Lunt, The UK contribution to paleoclimate modelling for CMIP6/ | + | |
- | * **Submitted** = //No// | + | |
- | * **Keywords** = // | + | |
- | * **Details** = The aim of this paper is to compare the MH and LIG HadGEM3 simulations, | + | |
- | * **Why** = The paper has direct relevance to various chapters/ | + | |
- | + | ||
- | * Charles JR Williams*, Dan Lunt, William Roberts, Alistair Sellars, CMIP6/ | + | |
- | * **Submitted** = //No// | + | |
- | * **Keywords** = // | + | |
- | * **Details** = The aim of this paper was to carry out a number of sensitivity experiments during the early Eocene using HadGEM3, to test the climate sensitivity (and particular hydro-climate e.g. changing precipitation patterns) to varying CO2 levels as well as a modified land sea mask and pole-equator SST changes | + | |
- | * **Why** = The paper has direct relevance to various chapters/ | + | |
- | + | ||
- | * Charles JR Williams*, Dan Lunt, William Roberts, Alistair Sellars, Alex Farnsworth, Fully-coupled early Eocene simulation using HadGEM3 as part of CMIP6/ | + | |
- | * **Submitted** = //No// | + | |
- | * **Keywords** = // | + | |
- | * **Details** = The aim of this paper was to conduct the fully coupled early Eocene simulation using HadGEM3, presenting both the experimental design and results based on model-model comparisons (e.g. with other Eocene simulations) and model-data comparisons | + | |
- | * **Why** = The paper has direct relevance to various chapters/ | + | |
- | + | ||
- | * Charles JR Williams*, Dan Lunt, William Roberts, Alistair Sellars, Fully-coupled Pliocene simulation using HadGEM3 as part of CMIP6/ | + | |
- | * **Submitted** = //No// | + | |
- | * **Keywords** = // | + | |
- | * **Details** = The aim of this paper was to conduct the fully coupled Pliocene simulation using HadGEM3, presenting both the experimental design and results based on model-model comparisons (e.g. with other Eocene simulations) and model-data comparisons. | + | |
- | * **Why** = The paper has direct relevance to various chapters/ | + | |
- | + | ||
- | + | ||
- | ===== Chapter 2: Changing state of the climate system ===== | + | |
- | + | ||
- | Number of selected references: **9** | + | |
* Kira Rehfeld*, Chris Brierley, Raphael Hebert, Juan Lora, Marcus Lovferstrom, | * Kira Rehfeld*, Chris Brierley, Raphael Hebert, Juan Lora, Marcus Lovferstrom, | ||
Line 53: | Line 16: | ||
* **Details** = n/a | * **Details** = n/a | ||
* **Why** = It looks at interannual variability in surface temperature and precipitation across both past and future simulations. It compares these response to existing compilations from palaeoclimate reconstructions. It also contains scatterplots of modes of climate variability (e.g. ENSO, IOD) to global temperature changes, and scaling diagnostics. | * **Why** = It looks at interannual variability in surface temperature and precipitation across both past and future simulations. It compares these response to existing compilations from palaeoclimate reconstructions. It also contains scatterplots of modes of climate variability (e.g. ENSO, IOD) to global temperature changes, and scaling diagnostics. | ||
+ | * **Suggested chapters** = 2, 4 | ||
+ | |||
+ | |||
* The ENSO gang at Past2Future.org, | * The ENSO gang at Past2Future.org, | ||
Line 59: | Line 25: | ||
* **Details** = This publication will look at the ENSO response during the Last Glacial, Mid-Holocene & Last Interglacial, | * **Details** = This publication will look at the ENSO response during the Last Glacial, Mid-Holocene & Last Interglacial, | ||
* **Why** = ENSO | * **Why** = ENSO | ||
+ | * **Suggested chapters** = 2 | ||
+ | |||
+ | |||
+ | |||
+ | * Dmitry Yumashev* & Chris Brierley, The economic implications of using the true preindustrial climate baseline | ||
+ | * **Submitted** = //No// | ||
+ | * **Keywords** = //early industrial vs preindustrial// | ||
+ | * **Details** = This paper will look at the cost-benefit analysis of using a preindustrial or early-industrial baseline. Whilst these may be statistically equivalent, which one is picked could still cause differences between different economic blocs. | ||
+ | * **Why** = This wil be relevant for the cross-chapter box on preindustrial definitions. It's analysis demonstrates that even a choice as scientifically arbitrary as this has social justice implications. It also states that this difference only matters if the Paris Agreement is met, and so shouldn' | ||
+ | * **Suggested chapters** = 1 | ||
+ | |||
+ | |||
* Cao, Jian; Wang, Bin; Liu,Jian, Attribution of the Last Glacial Maximum climate formation | * Cao, Jian; Wang, Bin; Liu,Jian, Attribution of the Last Glacial Maximum climate formation | ||
Line 65: | Line 43: | ||
* **Details** = n/a | * **Details** = n/a | ||
* **Why** = Attributed the contribution of each external forcing in the LGM temperature and precipitation change | * **Why** = Attributed the contribution of each external forcing in the LGM temperature and precipitation change | ||
+ | * **Suggested chapters** = 2, 8 | ||
+ | |||
+ | |||
* Cao, Jian; Wang, Bin; Ma, Libin, Attribution of Global Monsoon Response to the Last Glacial Maximum Forcings | * Cao, Jian; Wang, Bin; Ma, Libin, Attribution of Global Monsoon Response to the Last Glacial Maximum Forcings | ||
Line 71: | Line 52: | ||
* **Details** = The impact of LGM forcings to global monsoon precipitation changes over global or hemispheric scale. | * **Details** = The impact of LGM forcings to global monsoon precipitation changes over global or hemispheric scale. | ||
* **Why** = n/a | * **Why** = n/a | ||
+ | * **Suggested chapters** = 2, 4, 10 | ||
+ | |||
+ | |||
* Alexandre Cauquoin, Martin Werner*, Gerrit Lohmann, Water isotopes - climate relationships for the mid-Holocene and pre-industrial period simulated with an isotope-enabled version of MPI-ESM | * Alexandre Cauquoin, Martin Werner*, Gerrit Lohmann, Water isotopes - climate relationships for the mid-Holocene and pre-industrial period simulated with an isotope-enabled version of MPI-ESM | ||
Line 77: | Line 61: | ||
* **Details** = Paper currently in discussion at Climate of the Past: https:// | * **Details** = Paper currently in discussion at Climate of the Past: https:// | ||
* **Why** = The paper shows the first results, for the pre-industrial and mid-Holocene climatological periods, of the newly developed isotope-enhanced version of the fully coupled Earth system model MPI-ESM. The simulations follow the CMIP6-PMIP4 protocol and enable an improved model-data comparison for the mid-Holocene climate period. | * **Why** = The paper shows the first results, for the pre-industrial and mid-Holocene climatological periods, of the newly developed isotope-enhanced version of the fully coupled Earth system model MPI-ESM. The simulations follow the CMIP6-PMIP4 protocol and enable an improved model-data comparison for the mid-Holocene climate period. | ||
+ | * **Suggested chapters** = 2 | ||
- | * Charles J.R. Williams*, Maria V. Guarino, Joy S. Singarayer, Louise Sime, Emilie Capron, Daniel Lunt, The UK contribution to paleoclimate modelling for CMIP6/ | ||
- | * **Submitted** = //No// | ||
- | * **Keywords** = // | ||
- | * **Details** = The aim of this paper is to compare the MH and LIG HadGEM3 simulations, | ||
- | * **Why** = The paper has direct relevance to various chapters/ | ||
- | * Charles JR Williams*, Dan Lunt, William Roberts, Alistair Sellars, CMIP6/ | ||
- | * **Submitted** = //No// | ||
- | * **Keywords** = // | ||
- | * **Details** = The aim of this paper was to carry out a number of sensitivity experiments during the early Eocene using HadGEM3, to test the climate sensitivity (and particular hydro-climate e.g. changing precipitation patterns) to varying CO2 levels as well as a modified land sea mask and pole-equator SST changes | ||
- | * **Why** = The paper has direct relevance to various chapters/ | ||
- | * Charles JR Williams*, Dan Lunt, William Roberts, Alistair Sellars, Alex Farnsworth, Fully-coupled early Eocene simulation using HadGEM3 as part of CMIP6/ | + | * Quentin Dalaiden*, Hugues Goosse, François Klein, Jan T. M. Lenaerts, Max Holloway, Louise Sime, and Elizabeth R. Thomas, How is Antarctic snow accumulation useful in reconstructing surface temperature ? |
- | * **Submitted** = //No// | + | * **Submitted** = //Yes// |
- | * **Keywords** = //Paleoclimate modelling, early Eocene, experimental design, model-data comparisons// | + | * **Keywords** = //Surface temperature, snow accumulation, climate modelling, data assimilation// |
- | * **Details** = The aim of this paper was to conduct | + | * **Details** = The initial title is " |
- | * **Why** = The paper has direct relevance to various chapters/ | + | * **Why** = We show that snow accumulation is a more relevant proxy for Antarctic surface temperature reconstructions than delta18O. Based on a data assimilation method, our continental temperature reconstruction outperforms reconstructions based on delta18O, especially for East Antarctica. |
+ | * **Suggested chapters** = 9 | ||
- | * Charles JR Williams*, Dan Lunt, William Roberts, Alistair Sellars, Fully-coupled Pliocene simulation using HadGEM3 as part of CMIP6/ | ||
- | * **Submitted** = //No// | ||
- | * **Keywords** = // | ||
- | * **Details** = The aim of this paper was to conduct the fully coupled Pliocene simulation using HadGEM3, presenting both the experimental design and results based on model-model comparisons (e.g. with other Eocene simulations) and model-data comparisons. | ||
- | * **Why** = The paper has direct relevance to various chapters/ | ||
- | ===== Chapter 3: Human influence on the climate system ===== | + | |
- | + | ||
- | Number of selected references: **1** | + | |
- | + | ||
- | | + | |
* **Submitted** = //No// | * **Submitted** = //No// | ||
- | * **Keywords** = //Last Glacial Maximum, Holocene, 21st century// | + | * **Keywords** = //Monsoons midHolocene rcp8.5 PMIP3 CMIP5 past2future// |
- | * **Details** = This study describes the time evolution of near-surface air temperature in southern South America from the Last Glacial Maximum to the end of the 21st century based on PMIP3-CMIP5 model simulations. The study shows temperature changes throughout time and model simulations allow comparisons between climate changes occurred | + | * **Details** = n/a |
- | * **Why** = Model simulations suggest that the regional warming in response to anthropogenic forcings from 1850 to the end of the 21st century will be almost similar or even higher than the increment of temperature occurred between LGM and pre-Industrial times. | + | * **Why** = This paper highlights difference and analogies |
+ | * **Suggested chapters** = 8, 10 | ||
- | ===== Chapter 4: Future global climate: scenario-based projections and near-term information ===== | ||
- | Number of selected references: | + | |
- | + | ||
- | * Kira Rehfeld*, Chris Brierley, Raphael Hebert, Juan Lora, Marcus Lovferstrom, Variability of surface climate in PMIP3-PMIP4 simulations for past and future climate | + | |
* **Submitted** = //No// | * **Submitted** = //No// | ||
- | * **Keywords** = //interannual variability// | + | * **Keywords** = //Mediterranean, |
* **Details** = n/a | * **Details** = n/a | ||
- | * **Why** = It looks at interannual variability in surface temperature and precipitation across both past and future simulations. It compares these response to existing compilations from palaeoclimate reconstructions. It also contains scatterplots of modes of climate variability (e.g. ENSO, IOD) to global temperature changes, and scaling diagnostics. | + | * **Why** = This study analyses |
- | + | * **Suggested chapters** = 8, 10 | |
- | * Cao, Jian; Wang, Bin; Ma, Libin, Attribution of Global Monsoon Response to the Last Glacial Maximum Forcings | + | |
- | * **Submitted** = //Yes// | + | |
- | * **Keywords** = //LGM. global monsoon// | + | |
- | * **Details** = The impact of LGM forcings to global monsoon precipitation changes over global or hemispheric scale. | + | |
- | * **Why** = n/a | + | |
- | + | ||
- | * Gabriel Silvestri (*), Ana Laura Berman and Marcela Tonello, Modern anthropogenic warming in the context of past climate changes in southern South America | + | |
- | * **Submitted** = //No// | + | |
- | * **Keywords** = //Last Glacial Maximum, Holocene, 21st century// | + | |
- | * **Details** = This study describes | + | |
- | * **Why** = Model simulations suggest that the regional warming | + | |
- | + | ||
- | + | ||
- | ===== Chapter | + | |
- | + | ||
- | Number of selected references: **1** | + | |
- | + | ||
- | * Fabrice Lambert(*), N. Opazo, A. Ridgwell, G. Winckler, F. Lamy, G. Shaffer, K. Kohfeld, R. Ohgaito, S. Albani, A. Abe-Ouchi , Spatial | + | |
- | * **Submitted** = //No// | + | |
- | * **Keywords** = //iron fertilization co2// | + | |
- | * **Details** = Regional quantification of CO2 drawdown through iron fertilization | + | |
- | * **Why** = Gives an idea of the amount | + | |
- | + | ||
- | + | ||
- | ===== Chapter 6: Short-Lived Climate Forcers ===== | + | |
- | + | ||
- | Number of selected references: **1** | + | |
- | + | ||
- | * Fabrice Lambert(*), N. Opazo, A. Ridgwell, G. Winckler, F. Lamy, G. Shaffer, K. Kohfeld, R. Ohgaito, S. Albani, A. Abe-Ouchi , Spatial and Temporal Distribution of Ocean Iron Fertilization and CO2 drawdown during the Last Glacial Termination | + | |
- | * **Submitted** = //No// | + | |
- | * **Keywords** = //iron fertilization co2// | + | |
- | * **Details** = Regional quantification of CO2 drawdown through iron fertilization in individual HNLC regions | + | |
- | * **Why** = Gives an idea of the amount of CO2 that could be removed from the atmosphere through increased dust emissions in East Asia | + | |
- | ===== Chapter 7: The Earth' | ||
- | Number of selected references: **4** | ||
* Charles J.R. Williams*, Maria V. Guarino, Joy S. Singarayer, Louise Sime, Emilie Capron, Daniel Lunt, The UK contribution to paleoclimate modelling for CMIP6/ | * Charles J.R. Williams*, Maria V. Guarino, Joy S. Singarayer, Louise Sime, Emilie Capron, Daniel Lunt, The UK contribution to paleoclimate modelling for CMIP6/ | ||
Line 168: | Line 97: | ||
* **Details** = The aim of this paper is to compare the MH and LIG HadGEM3 simulations, | * **Details** = The aim of this paper is to compare the MH and LIG HadGEM3 simulations, | ||
* **Why** = The paper has direct relevance to various chapters/ | * **Why** = The paper has direct relevance to various chapters/ | ||
+ | * **Suggested chapters** = 1, 2, 7, 8, 9 | ||
+ | |||
+ | |||
* Charles JR Williams*, Dan Lunt, William Roberts, Alistair Sellars, CMIP6/ | * Charles JR Williams*, Dan Lunt, William Roberts, Alistair Sellars, CMIP6/ | ||
Line 174: | Line 106: | ||
* **Details** = The aim of this paper was to carry out a number of sensitivity experiments during the early Eocene using HadGEM3, to test the climate sensitivity (and particular hydro-climate e.g. changing precipitation patterns) to varying CO2 levels as well as a modified land sea mask and pole-equator SST changes | * **Details** = The aim of this paper was to carry out a number of sensitivity experiments during the early Eocene using HadGEM3, to test the climate sensitivity (and particular hydro-climate e.g. changing precipitation patterns) to varying CO2 levels as well as a modified land sea mask and pole-equator SST changes | ||
* **Why** = The paper has direct relevance to various chapters/ | * **Why** = The paper has direct relevance to various chapters/ | ||
+ | * **Suggested chapters** = 1, 2, 7 | ||
+ | |||
+ | |||
* Charles JR Williams*, Dan Lunt, William Roberts, Alistair Sellars, Alex Farnsworth, Fully-coupled early Eocene simulation using HadGEM3 as part of CMIP6/ | * Charles JR Williams*, Dan Lunt, William Roberts, Alistair Sellars, Alex Farnsworth, Fully-coupled early Eocene simulation using HadGEM3 as part of CMIP6/ | ||
Line 180: | Line 115: | ||
* **Details** = The aim of this paper was to conduct the fully coupled early Eocene simulation using HadGEM3, presenting both the experimental design and results based on model-model comparisons (e.g. with other Eocene simulations) and model-data comparisons | * **Details** = The aim of this paper was to conduct the fully coupled early Eocene simulation using HadGEM3, presenting both the experimental design and results based on model-model comparisons (e.g. with other Eocene simulations) and model-data comparisons | ||
* **Why** = The paper has direct relevance to various chapters/ | * **Why** = The paper has direct relevance to various chapters/ | ||
+ | * **Suggested chapters** = 1, 2, 7, 8, 9 | ||
- | * Charles JR Williams*, Dan Lunt, William Roberts, Alistair Sellars, Fully-coupled Pliocene simulation using HadGEM3 as part of CMIP6/ | ||
- | * **Submitted** = //No// | ||
- | * **Keywords** = // | ||
- | * **Details** = The aim of this paper was to conduct the fully coupled Pliocene simulation using HadGEM3, presenting both the experimental design and results based on model-model comparisons (e.g. with other Eocene simulations) and model-data comparisons. | ||
- | * **Why** = The paper has direct relevance to various chapters/ | ||
- | |||
- | ===== Chapter 8: Water Cycle Changes ===== | ||
- | |||
- | Number of selected references: **6** | ||
- | |||
- | * Cao, Jian; Wang, Bin; Liu,Jian, Attribution of the Last Glacial Maximum climate formation | ||
- | * **Submitted** = //Yes// | ||
- | * **Keywords** = //LGM, single forcing experiment// | ||
- | * **Details** = n/a | ||
- | * **Why** = Attributed the contribution of each external forcing in the LGM temperature and precipitation change | ||
- | |||
- | * Roberta D' | ||
- | * **Submitted** = //No// | ||
- | * **Keywords** = //Monsoons midHolocene rcp8.5 PMIP3 CMIP5 past2future// | ||
- | * **Details** = n/a | ||
- | * **Why** = This paper highlights difference and analogies on moisture budget components response (e.g. thermodynamics vs dynamics) in monsoon regions under orbital and greenhouse gas forcing. | ||
- | |||
- | * Roberta D' | ||
- | * **Submitted** = //No// | ||
- | * **Keywords** = // | ||
- | * **Details** = n/a | ||
- | * **Why** = This study analyses the hydrological cycle changes in the Mediterranean region in two climate scenarios: the LGM and rcp8.5. Moisture budget components (Thermodynamic, | ||
- | |||
- | * Charles J.R. Williams*, Maria V. Guarino, Joy S. Singarayer, Louise Sime, Emilie Capron, Daniel Lunt, The UK contribution to paleoclimate modelling for CMIP6/ | ||
- | * **Submitted** = //No// | ||
- | * **Keywords** = // | ||
- | * **Details** = The aim of this paper is to compare the MH and LIG HadGEM3 simulations, | ||
- | * **Why** = The paper has direct relevance to various chapters/ | ||
- | |||
- | * Charles JR Williams*, Dan Lunt, William Roberts, Alistair Sellars, Alex Farnsworth, Fully-coupled early Eocene simulation using HadGEM3 as part of CMIP6/ | ||
- | * **Submitted** = //No// | ||
- | * **Keywords** = // | ||
- | * **Details** = The aim of this paper was to conduct the fully coupled early Eocene simulation using HadGEM3, presenting both the experimental design and results based on model-model comparisons (e.g. with other Eocene simulations) and model-data comparisons | ||
- | * **Why** = The paper has direct relevance to various chapters/ | ||
* Charles JR Williams*, Dan Lunt, William Roberts, Alistair Sellars, Fully-coupled Pliocene simulation using HadGEM3 as part of CMIP6/ | * Charles JR Williams*, Dan Lunt, William Roberts, Alistair Sellars, Fully-coupled Pliocene simulation using HadGEM3 as part of CMIP6/ | ||
Line 227: | Line 124: | ||
* **Details** = The aim of this paper was to conduct the fully coupled Pliocene simulation using HadGEM3, presenting both the experimental design and results based on model-model comparisons (e.g. with other Eocene simulations) and model-data comparisons. | * **Details** = The aim of this paper was to conduct the fully coupled Pliocene simulation using HadGEM3, presenting both the experimental design and results based on model-model comparisons (e.g. with other Eocene simulations) and model-data comparisons. | ||
* **Why** = The paper has direct relevance to various chapters/ | * **Why** = The paper has direct relevance to various chapters/ | ||
+ | * **Suggested chapters** = 1, 2, 7, 8, 9 | ||
- | ===== Chapter 9: Ocean, Cryosphere, and Sea Level Change ===== | ||
- | Number of selected references: **4** | + | |
- | + | ||
- | * Quentin Dalaiden*, Hugues Goosse, François Klein, Jan T. M. Lenaerts, Max Holloway, Louise Sime, and Elizabeth R. Thomas, How is Antarctic snow accumulation useful in reconstructing surface temperature ? | + | |
- | | + | |
- | * **Keywords** = //Surface temperature, | + | |
- | * **Details** = The initial title is " | + | |
- | * **Why** = We show that snow accumulation is a more relevant | + | |
- | + | ||
- | * Charles J.R. Williams*, Maria V. Guarino, Joy S. Singarayer, Louise Sime, Emilie Capron, Daniel Lunt, The UK contribution to paleoclimate modelling for CMIP6/ | + | |
* **Submitted** = //No// | * **Submitted** = //No// | ||
- | * **Keywords** = //Paleaoclimate modelling, midHolocene, | + | * **Keywords** = //proxy-model integration, South America// |
- | * **Details** = The aim of this paper is to compare the MH and LIG HadGEM3 | + | * **Details** = This study summarizes difficulties concerning integrations |
- | * **Why** = The paper has direct relevance to various chapters/ | + | * **Why** = This study describes difficulties concerning evaluations of paleoclimatic |
- | * Charles JR Williams*, Dan Lunt, William Roberts, Alistair Sellars, Alex Farnsworth, Fully-coupled early Eocene simulation using HadGEM3 as part of CMIP6/ | ||
- | * **Submitted** = //No// | ||
- | * **Keywords** = // | ||
- | * **Details** = The aim of this paper was to conduct the fully coupled early Eocene simulation using HadGEM3, presenting both the experimental design and results based on model-model comparisons (e.g. with other Eocene simulations) and model-data comparisons | ||
- | * **Why** = The paper has direct relevance to various chapters/ | ||
- | * Charles JR Williams*, Dan Lunt, William Roberts, Alistair Sellars, Fully-coupled Pliocene simulation using HadGEM3 as part of CMIP6/ | + | * Gabriel Silvestri (*), Ana Laura Berman and Marcela Tonello, Modern anthropogenic warming in the context |
* **Submitted** = //No// | * **Submitted** = //No// | ||
- | * **Keywords** = //Paleoclimate modelling, Pliocene, experimental design, model-data comparisons// | + | * **Keywords** = //Last Glacial Maximum, Holocene, 21st century// |
- | * **Details** = The aim of this paper was to conduct | + | * **Details** = This study describes the time evolution |
- | * **Why** = The paper has direct relevance | + | * **Why** = Model simulations suggest that the regional warming in response |
+ | * **Suggested chapters** = 3, 4 | ||
- | ===== Chapter 10: Linking Global to Regional Climate Change ===== | ||
- | Number of selected references: | + | |
- | + | ||
- | * Cao, Jian; Wang, Bin; Ma, Libin, Attribution of Global Monsoon Response to the Last Glacial Maximum Forcings | + | |
- | * **Submitted** = //Yes// | + | |
- | * **Keywords** = //LGM. global monsoon// | + | |
- | * **Details** = The impact of LGM forcings to global monsoon precipitation changes over global or hemispheric scale. | + | |
- | * **Why** = n/a | + | |
- | + | ||
- | * Roberta D' | + | |
* **Submitted** = //No// | * **Submitted** = //No// | ||
- | * **Keywords** = //Monsoons midHolocene rcp8.5 PMIP3 CMIP5 past2future// | + | * **Keywords** = //iron fertilization co2// |
- | * **Details** = n/a | + | * **Details** = Regional quantification of CO2 drawdown through iron fertilization in individual HNLC regions |
- | * **Why** = This paper highlights difference and analogies on moisture budget components response (e.g. thermodynamics vs dynamics) | + | * **Why** = Gives an idea of the amount of CO2 that could be removed from the atmosphere through increased dust emissions |
- | + | * **Suggested chapters** = 5, 6 | |
- | * Roberta D' | + | |
- | * **Submitted** = //No// | + | |
- | * **Keywords** = // | + | |
- | * **Details** = n/a | + | |
- | * **Why** = This study analyses the hydrological cycle changes in the Mediterranean region in two climate scenarios: the LGM and rcp8.5. Moisture budget components (Thermodynamic, | + | |
- | + | ||
- | + | ||
- | ===== Chapter 11: Weather and Climate Extreme Events in a Changing Climate ===== | + | |
- | + | ||
- | Number of selected references: **0** | + | |
- | ===== Chapter 12: Climate change information for regional impacts and risk assessment ===== | ||
- | Number of selected references: **0** | ||