Climate Regime Building in a Changing World and China's Role in Global Climate Governance

Author(s):  
JIAHUA PAN ◽  
MOU WANG
2020 ◽  
Vol 20 (4) ◽  
pp. 122-142
Author(s):  
Ekaterina Domorenok ◽  
Giuseppe Acconcia ◽  
Lena Bendlin ◽  
Xira Ruiz Campillo

Over the last decade, a growing body of academic literature has reflected on how and under which conditions experiments in global climate governance lead to broader changes in rules, norms, and practices helping to meet the challenge of climate change. Drawing on the assumptions of the scholarship on experimentalist governance architectures, this article analyzes the effectiveness of the Covenant of Mayors (CoM) as a comprehensive governance framework that enables the development and coordination of local policies for sustainable energy and climate through a range of joint instruments for recursive goal setting, monitoring, and benchmarking. Our findings illustrate the CoM’s significant potential in terms of both general political uptake and policy output, which could make of this program, if appropriately fine-tuned, a successful governance experiment contributing to building a more effective global climate regime.


2012 ◽  
Author(s):  
Richard B. Stewart ◽  
Michael Oppenheimer ◽  
Bryce Rudyk

2013 ◽  
Vol 01 (01) ◽  
pp. 1350008 ◽  
Author(s):  
Mou WANG

Drawing on the idea that countries are eligible to implement differentiated emission reduction policies based on their respective capabilities, some parties of UNFCCC attempt to weaken the principle of “Common but differentiated responsibilities(CBDR)” and impose carbon tariff on international trade. This initiative is in fact another camouflage to burden developing countries with emission cut obligation, which has no doubt undermined the development rights of developing countries. This paper defines Carbon Tariff as border measures that target import goods with embodied carbon emission. It can be import tariffs or other domestic tax measures that adjust border tax, which includes plain import tariffs and export rebates, border tax adjustment, emission quota and permit etc. For some developed countries, carbon tariffs mean to sever trade protectionism and to build trade barriers. Its theoretical arguments like “loss of comparative advantage”, “carbon leakage decreases environmental effectiveness” and “theoretical model bases” are pseudo-propositions without international consensus. Carbon tariff has become an intensively debated issue due to its duality of climate change and trade, but neither UNFCCC nor WTO has clarified this issue or has indicated a clear statement in this regard. As a result, it allows some parties to take advantage of this loophole and escape its international climate change obligation. Carbon tariff is an issue arising from global climate governance. To promote the cooperation of global climate governance and safeguard the social and economic development of developing countries, a fair and justified climate change regime and international trade institution should be established, and the settlement of the carbon tariff issue should be addressed within these frameworks. This paper argues that the international governance of carbon tariff should in cooperation with other international agreements; however, principles and guidelines regarding this issue should be developed under the UNFCCC. Based on these principles and guidelines, WTO can develop related technical operation provisions.


2021 ◽  
Author(s):  
Christoph Braun ◽  
Aiko Voigt ◽  
Johannes Hörner ◽  
Joaquim G. Pinto

<p>Stable waterbelt climate states with close to global ice cover challenge the classical Snowball Earth hypothesis because they provide a robust explanation for the survival of advanced marine species during the Neoproterozoic glaciations (1000 – 541 Million years ago). Whether Earth’s climate stabilizes in a waterbelt state or rushes towards a Snowball state is determined by the magnitude of the ice-albedo feedback in the subtropics, where dark, bare sea ice instead of snow-covered sea ice prevails. For a given bare sea-ice albedo, the subtropical ice-albedo feedback and thus the stable range of the waterbelt climate regime is sensitive to the albedo over ice-free ocean, which is largely determined by shortwave cloud-radiative effects (CRE). In the present-day climate, CRE are known to dominate the spread of climate sensitivity across global climate models. We here study the impact of uncertainty associated with CRE on the existence of geologically relevant waterbelt climate regimes using two global climate models and an idealized energy balance model. We find that the stable range of the waterbelt climate regime is very sensitive to the abundance of subtropical low-level mixed-phase clouds. If subtropical cloud cover is low, climate sensitivity becomes so high as to inhibit stable waterbelt states.</p><p>The treatment of mixed-phase clouds is highly uncertain in global climate models. Therefore we aim to constrain the uncertainty associated with their CRE by means of a hierarchy of global and regional simulations that span horizontal grid resolutions from 160 km to 300m, and in particular include large eddy simulations of subtropical mixed-phase clouds located over a low-latitude ice edge. In the cold waterbelt climate subtropical CRE arise from convective events caused by strong meridional temperature gradients and stratocumulus decks located in areas of large-scale descending motion. We identify the latter to dominate subtropical CRE and therefore focus our large eddy simulations on subtropical stratocumulus clouds. By conducting simulations with two extreme scenarios for the abundance of atmospheric mineral dust, which serves as ice-nucleating particles and therefore can control mixed-phase cloud physics, we aim to estimate the possible spread of CRE associated with subtropical mixed-phase clouds. From this estimate we may assess whether Neoproterozoic low-level cloud abundance may have been high enough to sustain a stable waterbelt climate regime.</p>


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