climate transition
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2022 ◽  
pp. 297-361
Author(s):  
Simone Galeotti ◽  
Peter Bijl ◽  
Henk Brinkuis ◽  
Robert M. DeConto ◽  
Carlota Escutia ◽  
...  
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2021 ◽  
Author(s):  
Liu Yang ◽  
Jiaxi Tian ◽  
Yuanhai Fu ◽  
Bin Zhu ◽  
Xu He ◽  
...  

Abstract Whether there is a transition underway, from a warm-dry climate to a warm-wet climate in Northwest China remains a controversial and scientifically significant issue. Will this trend continue in the future? Another hot issue is whether the climate in Northwest China will continue to be warm and humid over the next few decades. In this paper, eight CMIP6 models were employed to investigate temperature and precipitation changes under five principal Shared Socioeconomic Pathway (SSP) scenarios (from 2015 to 2099) to project the future warming and humidification in Northwest China using the SPEI (standardized precipitation evapotranspiration index) method. The results revealed that (1) the simulated temperature and precipitation of eight CMIP6 models were consistent with that of observed data during 1961–2014, which showed an increase of approximately 28.2 mm, while simulated data revealed an increase of approximately 9.4 mm. The annual precipitation gradually decreased from Eastern Inner Mongolia and the Southern Northwest Mongolia region (>700 mm) to the Central Northwest Mongolia region (<100 mm) from 1961 to 2014; (2) the MME significantly overestimated the temperature and slightly underestimated the precipitation in Northwest Mongolia. The temperature difference between the simulated and observed data was approximately 0.4 °C. The observed data showed an increase of approximately 0.9 °C from 1961 to 2014, whereas the simulated data revealed an increase of approximately 0.7 °C; (3) in the SSP5-8.5 scenario, the percentage of precipitation anomalies at 1.5, 2, 3, and 4 °C were 166.64, 190.58, 226.44, and 274.56%, respectively; thus, alleviating the drought situation while facilitating the warm-dry to warm-wet climate transition; (4) the water balance between rising temperatures and increased evapotranspiration resulting from increased precipitation suggested that not all sites will be wet in the future. There was still a drying trend in some areas, where drought was more severe under the high emissions scenario than the low emissions scenario.


Agriculture ◽  
2021 ◽  
Vol 11 (12) ◽  
pp. 1248
Author(s):  
Giancarlo Bozzo ◽  
Marialaura Corrente ◽  
Giovanni Testa ◽  
Gaia Casalino ◽  
Michela Maria Dimuccio ◽  
...  

Climate change is internationally recognized as a source of concern by governments, scientists and public opinion. In this context, the need to find concrete solutions becomes increasingly urgent. Numerous economic sectors contribute to alteration of climate, especially livestock and, more generally, food production-related activities. For this reason, animal welfare policies, the complex of norms and regulations adopted by single Member States and the European Union in the field of meat production, could be a useful instrument in the climate transition invoked by policy makers and scientists. The aim of this paper was to analyze the current system of animal welfare from a legal and veterinary perspective, and to demonstrate how important and useful, it could be in the fight against climate change; at least if correctly implemented and applied.


2021 ◽  
Author(s):  
Bolin Sun ◽  
Long Ma ◽  
Tingxi Liu ◽  
Xing Huang

Abstract The overlap region between the eastern fringe of the Asian westerly region and the temperate continental-monsoon climate transition zone is sensitive to climate changes and is characterized by fragile ecosystems. It is necessary to uncover the patterns of long-term historical climate variability there. A standardized tree-ring width chronology was constructed based on the tree-ring samples collected from four representative tree species in four typical areas in the overlap region, and the 203- to 343-year annual mean minimum temperature series in the overlap region were reconstructed. The reconstructed series overlapped well with extreme climate events and low-temperature periods recorded in historical data. Therefore, the reconstructed model is stable and reliable. As suggested by the reconstructed series, the variability of annual mean minimum temperature was increasingly drastic from east to west in the overlap region, with gradually shorter periodicities. In the 19th century, the high-latitude area was in the high-temperature period, and the entire overlap region experienced significant low-temperature periods lasting 20–45 years till the 1950s. The western part had an earlier start time of low-temperature periods, longer cooling duration, and slower cooling rate than the central part. The overlap region experienced a significant warming period in approximately the last half-century, with temperature increasing faster in the western and eastern parts than in the central part. The temperature variability in the overlap region was more intense in the last two centuries, with shorter periodicities and a larger proportion of cold periods. The central and western parts of the Asian westerly region, the mid- to high-latitude regions of the transition zone, and the overlap region saw significantly low-temperature periods or drastic cooling trends (the Little Ice Age) in the first half of the 19th century and significant warming trends under global warming afterwards. The influences of these changes might have been exacerbated by the westerly circulation. This study not only provides new insight into the use of dendroclimatology to extract temperature series in the Asian westerly region and the transition zone but also serves as a reference for research on global climate change.


2021 ◽  
Vol 12 (1) ◽  
Author(s):  
Hong Ao ◽  
Eelco J. Rohling ◽  
Ran Zhang ◽  
Andrew P. Roberts ◽  
Ann E. Holbourn ◽  
...  

AbstractAcross the Miocene–Pliocene boundary (MPB; 5.3 million years ago, Ma), late Miocene cooling gave way to the early-to-middle Pliocene Warm Period. This transition, across which atmospheric CO2 concentrations increased to levels similar to present, holds potential for deciphering regional climate responses in Asia—currently home to more than half of the world’s population— to global climate change. Here we find that CO2-induced MPB warming both increased summer monsoon moisture transport over East Asia, and enhanced aridification over large parts of Central Asia by increasing evaporation, based on integration of our ~1–2-thousand-year (kyr) resolution summer monsoon records from the Chinese Loess Plateau aeolian red clay with existing terrestrial records, land-sea correlations, and climate model simulations. Our results offer palaeoclimate-based support for ‘wet-gets-wetter and dry-gets-drier’ projections of future regional hydroclimate responses to sustained anthropogenic forcing. Moreover, our high-resolution monsoon records reveal a dynamic response to eccentricity modulation of solar insolation, with predominant 405-kyr and ~100-kyr periodicities between 8.1 and 3.4 Ma.


Author(s):  
Thomas B. Long ◽  
Vincent Blok

AbstractGreen New Deal (GND) policies are proposed to tackle the climate emergency. These policies focus on driving climate innovation through unprecedented financial policy levers. However, while the macro-level financing dynamics are clear, the influence of niche level dynamics of sustainable innovation financing remain unexplored within these policy settings. Through the context of the European Green Deal and a focus on the agri-tech start-up sector in the Netherlands, we identify factors likely to reduce the efficacy of these policies from an innovation management perspective—such as project matching issues, socio-ethical factors or the characteristics of agri-food climate innovations. We go on to conceptualise that these challenges represent a range of asymmetries—from classic information asymmetries to less common value and objective asymmetries—between climate innovators and private investors and financers. Many remedies for asymmetries involve costs, likely to further inhibit the efficacy of the European Green Deal and similar policies. A partnering approach is proposed, where the non-financial resources of incumbent actors are harnessed and leveraged to enhance climate innovation performance.


2021 ◽  
pp. 1-20
Author(s):  
Shijun Song ◽  
Lei Huang ◽  
Yongshu Zhang ◽  
Qi Zhang ◽  
Fei Zhou ◽  
...  

Abstract The Middle Miocene Climatic Optimum is known for abrupt events during the global cooling trend of the past 20 Ma. Its identification in the Tibetan Plateau can help explain the cause of the critical Middle Miocene climate transition in Central Asia. In this study, fine-grained mixed sediments widely distributed in the Miocene Qaidam Lake in the northern Tibetan Plateau were used as a sensitive indicator for palaeoclimate. Their geochemical characteristics were investigated, together with an analysis of 2600 m long successive gamma-ray logging data from the whole JS2 drillcore, to understand the mid-Miocene climate transition in the Tibetan Plateau. By comparing the gamma-ray curve of the mixed sediments with global temperature, the Middle Miocene Climatic Optimum event can be easily identified. Further, the detailed petrological features and geochemical data of lacustrine fine-grained mixed sediments from a 400 m drillcore show oxidizing, high-sedimentation rate and brackish-saline water conditions in a semi-arid climate during the Middle Miocene period, demonstrating a dryer climate in the Qaidam Basin than in the monsoon-sensitive regions in Central Asia. These fine-grained mixed sediments have recorded climate drying before 15.3 Ma that represents a climatic transition within the Middle Miocene Climatic Optimum; increasing carbonate-rich mixed sediments, decreasing algal limestone layers and decreasing lacustrine organic matter are indicators of this transition. Regional tectonic events include the retreat of the Paratethys from Central Asia at ∼15 Ma and the synchronous tectonic reorganization of the Altyn-Tagh fault system and the northeastern Tibetan Plateau. We find that global climate change is the primary factor affecting the overall characteristics and changes of the Neogene climate in the Qaidam Basin, including the occurrence of the Middle Miocene Climatic Optimum and the cooling and drying tendency, while the regional events are a secondary factor.


2021 ◽  
Vol 17 (5) ◽  
pp. 2255-2271
Author(s):  
Thomas J. Leutert ◽  
Sevasti Modestou ◽  
Stefano M. Bernasconi ◽  
A. Nele Meckler

Abstract. The middle Miocene climate transition (MMCT), around 14 Ma, was associated with a significant climatic shift, but the mechanisms triggering the event remain enigmatic. We present a clumped isotope (Δ47) bottom-water temperature (BWT) record from 16.0 to 12.2 Ma from Ocean Drilling Program (ODP) Site 747 in the Southern Ocean and compare it to existing BWT records from different latitudes. We show that BWTs in the Southern Ocean reached 8–10 ∘C during the Miocene climatic optimum. These high BWT values indicate considerably warmer bottom-water conditions than today. Nonetheless, bottom-water δ18O (calculated from foraminiferal δ18O and Δ47) suggests substantial amounts of land ice throughout the interval of the study. Our dataset further demonstrates that BWTs at Site 747 were variable with an overall cooling trend across the MMCT. Notably, a cooling of around 3–5 ∘C preceded the stepped main increase in benthic δ18O, interpreted as global ice volume expansion, and appears to have been followed by a transient bottom-water warming starting during or slightly after the main ice volume increase. We speculate that a regional freshening of the upper water column at this time may have increased stratification and reduced bottom-water heat loss to the atmosphere, counteracting global cooling in the bottom waters of the Southern Ocean and possibly even at larger scales. Feedbacks required for substantial ice growth and/or tectonic processes may have contributed to the observed decoupling of global ice volume and Southern Ocean BWT.


2021 ◽  
Author(s):  
Reinis Āzis

The topics covered and the research framework as such provide multiple level takeaways regarding energy efficiency and climate neutrality. The research, therefore, elaborates on concepts central to the academic debate at the time of the writing and undercuts patterns and proposals relevant for multiple actors within the local and global energy market. In fact, the research develops broader discussion regarding any strategic energy-efficiency related goal and the complexity and multiple threads that meeting such a goal would entail. The research also explicitly elaborates on the role of energy efficiency in both climate transition and energy system transformation. In addition, it uncovers the scope of various policies implemented on a local level and discusses their role in meeting the climate targets in medium and long-term. Furthermore, the research also elaborates on the role of bioeconomy and climate neutrality.


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