Chapter 3. From the Berlin Mandate to the Kyoto Protocol (1995–1997): EU Influence on the First Development of the Global Climate Regime

2016 ◽  
Keyword(s):  
Kyoto Protocol ◽  
Global Climate ◽  
Climate Regime

scholarly journals Reshaping the Global Climate Change Regime through the Paris Agreement

2017 ◽  
Vol 6 (2) ◽  
pp. 1-32
Author(s):  
Theodore Okonkwo
Keyword(s):  
Climate Change ◽  
Kyoto Protocol ◽  
Global Climate ◽  
Paris Agreement ◽  
Climate Regime ◽  
Common But Differentiated Responsibilities ◽  
Copenhagen Accord ◽  
International Diplomacy ◽  
Cursory Examination ◽  
Combat Climate Change

The Paris Agreement on Climate Change which aimed at halting climate change and limiting global warming to 1.5 degrees Celsius, remains the most important piece of international diplomacy in years, since the Kyoto Protocol of 1992 and the Copenhagen Accord (which endorsed the continuation of the Kyoto Protocol) 2009. The signing of the Paris Agreement underlies the fact that climate change remains one of the greatest challenges of our time and calls for a strong political will to urgently combat climate change in accordance with the principle of common but differentiated responsibilities and respective capabilities. This article looks at Paris Agreement’s resolve to peak global greenhouse-gas emissions as soon as possible and also undertakes a cursory examination of the global climate regime. The article also examines how the problem of climate change has altered since the 2009 Copenhagen Accord and concludes by emphasizing the need to take the Paris Agreement forward in spirit.

Building a More Effective Global Climate Regime Bottom-Up

2012 ◽  
Author(s):  
Richard B. Stewart ◽  
Michael Oppenheimer ◽  
Bryce Rudyk
Keyword(s):  
Global Climate ◽  
Climate Regime ◽  
Bottom Up

Constraining Neoproterozoic subtropical low-level clouds to assess the plausibility of near-Snowball Earth states

2021 ◽  
Author(s):  
Christoph Braun ◽  
Aiko Voigt ◽  
Johannes Hörner ◽  
Joaquim G. Pinto
Keyword(s):  
Sea Ice ◽  
Climate Models ◽  
Global Climate ◽  
Global Climate Models ◽  
Mixed Phase ◽  
Snowball Earth ◽  
Stable Range ◽  
Climate Regime ◽  
Low Level ◽  
Mixed Phase Clouds

<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>

EU Climate and Energy Policy: A Hesitant Supranational Turn?

2012 ◽  
Vol 12 (2) ◽  
pp. 67-86 ◽  
Author(s):  
Jørgen Wettestad ◽  
Per Ove Eikeland ◽  
Måns Nilsson
Keyword(s):  
European Commission ◽  
Energy Policy ◽  
Vertical Integration ◽  
Energy Security ◽  
Emissions Trading ◽  
Global Climate ◽  
Energy Market ◽  
Climate Regime ◽  
Regional Energy ◽  
Climate And Energy Policy

This article examines the recent changes of three central EU climate and energy policies: the revised Emissions Trading Directive (ETS); the Renewables Directive (RES); and internal energy market (IEM) policy. An increasing transference of competence to EU level institutions, and hence “vertical integration,” has taken place, most clearly in the case of the ETS. The main reasons for the differing increase in vertical integration are, first, that more member states were dissatisfied with the pre-existing system in the case of the ETS than in the two other cases. Second, the European Commission and Parliament were comparatively more united in pushing for changes in the case of the ETS. And, third, although RES and IEM policies were influenced by regional energy security concerns, they were less structurally linked to and influenced by the global climate regime than the ETS.

Burden-sharing and global climate negotiations: the case of the Kyoto Protocol

2010 ◽  
Vol 10 (2) ◽  
pp. 131-147 ◽  
Author(s):  
YOSEF BHATTI ◽  
KASPER LINDSKOW ◽  
LENE HOLM PEDERSEN
Keyword(s):  
Kyoto Protocol ◽  
Global Climate ◽  
Burden Sharing ◽  
Climate Negotiations

scholarly journals The Paris Agreement: Historic Breakthrough or High Stakes Experiment?

Climate Law ◽  
2016 ◽  
Vol 6 (1-2) ◽  
pp. 1-20 ◽  
Author(s):  
Meinhard Doelle
Keyword(s):  
Kyoto Protocol ◽  
Paris Agreement ◽  
Climate Regime ◽  
Top Down ◽  
High Stakes ◽  
Flexible Approach ◽  
Climate Negotiations ◽  
Loss And Damage ◽  
Self Differentiation

This article offers an overview of the two key outcomes of the 2015 Paris climate negotiations, the Paris cop decision, and the Paris Agreement. Collectively, they chart a new course for the un climate regime that started in earnest in Copenhagen in 2009. The Paris Agreement represents a path away from the top-down approach and rigid differentiation among parties reflected in the Kyoto Protocol, toward a bottom-up and flexible approach focused on collective long-term goals and principles. It represents an approach to reaching these long-term goals that is focused on self-differentiation, support, transparency, and review. The article highlights the key elements of the agreement reached in Paris, including its approach to mitigation, adaptation, loss and damage, finance, transparency, and compliance.

scholarly journals The risk of carbon leakage in global climate agreements

2020 ◽  
Author(s):  
Tobias Nielsen ◽  
Nicolai Baumert ◽  
Astrid Kander ◽  
Magnus Jiborn ◽  
Viktoras Kulionis
Keyword(s):  
Climate Change ◽  
Kyoto Protocol ◽  
Global Climate ◽  
Developed Countries ◽  
Carbon Leakage ◽  
Policy Makers ◽  
Climate Agreements ◽  
Climate Action ◽  
The Usa ◽  
Nationally Determined Contributions

Abstract Although climate change and international trade are interdependent, policy-makers often address the two topics separately. This may inhibit progress at the intersection of climate change and trade and could present a serious constraint for global climate action. One key risk is carbon leakage through emission outsourcing, i.e. reductions in emissions in countries with rigorous climate policies being offset by increased emissions in countries with less stringent policies. We first analyze the Paris Agreement’s nationally determined contributions (NDC) and investigate how carbon leakage is addressed. We find that the risk of carbon leakage is insufficiently accounted for in these documents. Then, we apply a novel quantitative approach (Jiborn et al., 2018; Baumert et al., 2019) to analyze trends in carbon outsourcing related to a previous international climate regime—the Kyoto Protocol—in order to assess whether reported emission reductions were offset by carbon outsourcing in the past. Our results for 2000–2014 show a more nuanced picture of carbon leakage during the Kyoto Protocol than previous studies have reported. Carbon outsourcing from developed to developing countries was dominated by the USA outsourcing to China, while the evidence for other developed countries was mixed. Against conventional wisdom, we find that, in general, countries that stayed committed to their Kyoto Protocol emission targets were either only minor carbon outsourcers or actually even insourcers—although the trend was slightly negative—indicating that binding emissions targets do not necessarily lead to carbon outsourcing. We argue that multiple carbon monitoring approaches are needed to reduce the risk of carbon leakage.

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