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Surface temperatures increase at a greater rate over land than ocean in simulations and observations of global warming. It has previously been proposed that this land–ocean warming contrast is related to different changes in lapse rates over land and ocean because of limited moisture availability over land. A simple theory of the land–ocean warming contrast is developed here in which lapse rates are determined by an assumption of convective quasi-equilibrium. The theory predicts that the difference between land and ocean temperatures increases monotonically as the climate warms or as the land becomes more arid. However, the ratio of differential warming over land and ocean varies nonmonotonically with temperature for constant relative humidities and reaches a maximum at roughly 290 K.

The theory is applied to simulations with an idealized general circulation model in which the continental configuration and climate are varied systematically. The simulated warming contrast is confined to latitudes below 508 when climate is varied by changes in longwave optical thickness. The warming contrast depends on land aridity and is larger for zonal land bands than for continents with finite zonal extent. A land–ocean temperature contrast may be induced at higher latitudes by enforcing an arid land surface, but its magnitude is relatively small. The warming contrast is generally well described by the theory, although inclusion of a land– ocean albedo contrast causes the theory to overestimate the land temperatures. Extensions of the theory are discussed to include the effect of large-scale eddies on the extratropical thermal stratification and to account for warming contrasts in both surface air and surface skin temperatures.

© 2013 American Meteorological Society

With federal policies to curb greenhouse gas emissions in the U.S. stagnating, California has taken action on its own. We estimate the impact of California’s cap-and-trade program on the leakage of emissions to other regions using a calibrated general equilibrium model. Sub-national policies can lead to high leakage rates as state economies are generally closely connected to other economies, including integration of electricity markets. Measures that will prevent leakage from California’s cap-and-trade program include requiring permits to be surrendered for emissions embodied in imported electricity and legislation banning “resource shuffling”. Under a cap-and-trade policy without measures to reduce leakage, the price of emission permits is $12 per ton of CO2 and emissions in other regions increase by 46% of the reduction in emissions in California. When imported electricity is included in the program and resource shuffling is banned, the carbon price is $65, there is negative leakage to regions exporting electricity to California, positive leakage to other regions and the overall leakage rate is 2%. We conclude that although there is potential for large increases in emissions elsewhere due to California’s cap-and-trade policy, enforcement of requirements for imported electricity will be effective at curtailing leakage.

With federal policies to curb carbon emissions stagnating in the U.S., California is taking action alone. Sub-national policies can lead to high rates of emissions leakage to other regions as state-level economies are closely connected, including integration of electricity markets. Using a calibrated general equilibrium model, we estimate that California's cap-and-trade program without restrictions on imported electricity increases out-of-state emissions by 45% of the domestic reduction. When imported electricity is included in the cap and "resource shuffling" is banned, as set out in California's legislation, emissions reductions in electricity exporting states partially offset leakage elsewhere and overall leakage is 9%.

© 2014 International Association for Energy Economics

In the negotiations of the United Nations Framework Convention on Climate Change (UNFCCC), new market mechanisms are proposed to involve Non-Annex I countries in the carbon markets developed by Annex I countries, beyond their current involvement through the Clean Development Mechanism (CDM). Sectoral trading is one such mechanism. It would consist of coupling one economic sector of a Non-Annex I country, e.g., the Chinese electricity sector, with the carbon market of some Annex I countries, e.g., the European Union Emission Trading Scheme (EU ETS). Previous research analyzed the potential impacts of such a mechanism and concluded that a limit would likely be set on the amount of carbon permits that could be imported from the non-Annex I country to the Annex I carbon market, should such a mechanism come into effect. This paper analyzes the impact of limited trading in carbon permits between the EU ETS and Chinese electricity sector when the latter is constrained by a 10% emissions reduction target below business as usual by 2030. The limit on the amount of Chinese carbon permits that could be sold into the European carbon market is modeled through the introduction of a trade certificate system. The analysis employs the MIT Emissions Prediction and Policy Analysis (EPPA) model and takes into account the banking–borrowing of allowances and the inclusion of aviation emissions in the EU ETS. We find that if the amount of permits that can be imported from China to Europe is 10% of the total amount of European allowances, the European carbon price decreases by 34%, while it decreases by 74 % when sectoral trading is not limited. As a consequence, limited sectoral trading does not reverse the changes initiated in the European electricity sector as much as unlimited sectoral trading would. We also observe that international leakage and leakage to non-electricity sectors in China are lower under limited sectoral trading, thus achieving more emissions reductions at the aggregate level. Finally, we find that, if China can capture the rents due to the limit on sectoral trading, it is possible to find a limit that makes both regions better off relative to when there is no international trade in carbon permits.

Simulations of warming climates with coupled climate models exhibit strong land-ocean contrasts in changes in surface temperature and relative humidity, but little land-ocean contrast in changes in equivalent potential temperature. A theory that assumes equal changes in equivalent potential temperature over land and ocean captures the simulated land-ocean warming contrast in the tropics if changes in relative humidity and ocean temperature are taken as given. According to the theory, land relative humidity changes and the land-ocean contrast in the control climate contribute equally to the tropical warming contrast, while ocean relative humidity changes make a smaller (but also positive) contribution. Intermodel scatter in the tropical warming contrast is primarily linked to land relative humidity changes. These results emphasize the need to better constrain land relative humidity changes in model simulations, and they are also relevant for changes in heat stress over land.

© 2013 American Geophysical Union

We use the global 3-D chemical transport model GEOS-Chem to simulate long-range atmospheric transport of polycyclic aromatic hydrocarbons (PAHs). To evaluate the model’s ability to simulate PAHs with different volatilities, we conduct analyses for phenanthrene (PHE), pyrene (PYR), and benzo[a]pyrene (BaP). GEOS-Chem captures observed seasonal trends with no statistically significant difference between simulated and measured mean annual concentrations. GEOS-Chem also captures variability in observed concentrations at nonurban sites (r = 0.64, 0.72, and 0.74, for PHE, PYR, and BaP). Sensitivity simulations suggest snow/ice scavenging is important for gas-phase PAHs, and on-particle oxidation and temperature-dependency of gas-particle partitioning have greater effects on transport than irreversible partitioning or increased particle concentrations. GEOS-Chem estimates mean atmospheric lifetimes of <1 day for all three PAHs. Though corresponding half-lives are lower than the 2-day screening criterion for international policy action, we simulate concentrations at the high-Arctic station of Spitsbergen within four times observed concentrations with strong correlation (r = 0.70, 0.68, and 0.70 for PHE, PYR, and BaP). European and Russian emissions combined account for ∼80% of episodic high-concentration events at Spitsbergen.

© 2012 American Chemical Society

This paper summarizes the results of an intercomparison project with Earth System Models of Intermediate Complexity (EMICs) undertaken in support of the Intergovernmental Panel on Climate Change (IPCC) Fifth Assessment Report (AR5). The focus is on long-term climate projections designed to 1) quantify the climate change commitment of different radiative forcing trajectories and 2) explore the extent to which climate change is reversible on human time scales. All commitment simulations follow the four representative concentration pathways (RCPs) and their extensions to year 2300. Most EMICs simulate substantial surface air temperature and thermosteric sea level rise commitment following stabilization of the atmospheric composition at year-2300 levels. The meridional overturning circulation (MOC) is weakened temporarily and recovers to near-preindustrial values in most models for RCPs 2.6–6.0. The MOC weakening is more persistent for RCP8.5. Elimination of anthropogenic CO2 emissions after 2300 results in slowly decreasing atmospheric CO2 concentrations. At year 3000 atmospheric CO2 is still at more than half its year-2300 level in all EMICs for RCPs 4.5–8.5. Surface air temperature remains constant or decreases slightly and thermosteric sea level rise continues for centuries after elimination of CO2 emissions in all EMICs. Restoration of atmospheric CO2 from RCP to preindustrial levels over 100–1000 years requires large artificial removal of CO2 from the atmosphere and does not result in the simultaneous return to preindustrial climate conditions, as surface air temperature and sea level response exhibit a substantial time lag relative to atmospheric CO2.

© 2013 American Meteorological Society

This thesis addresses the question of how to maximize the value of energy capital projects in light of the various risks faced by these projects. The risks can be categorized as exogenous risks (not in control of involved entities) and endogenous risks (arising from sub-optimal decisions by involved entities). A dominant reason for poor project performance is the endogenous risks associated with weak incentives to deliver optimal project outcomes. A key objective of this research is to illustrate that risk-sharing through contracts is central to incentivize the involved entities to maximize overall project value.

The thesis presents a risk management framework for energy capital projects that accounts for both exogenous risks and endogenous risks to evaluate the optimal risk management strategies. This work focuses on a carbon capture and storage project (CCS) with enhanced oil recovery (EOR). CCS is projected to play a key role in reducing the global CO2 emissions. However, the actual deployment of CCS is likely to be lower than projected because of the various risks and uncertainties involved. The analysis of CCS-EOR projects presented in this thesis will help encourage the commercial deployment of CCS by identifying the optimal risk management strategies. This work analyzes the impact of the exogenous risks (market risks, geological uncertainty) on the value of the CCS-EOR project, and evaluates the optimal contingent decisions. Endogenous risks arise from the involvement of multiple entities in the CCS-EOR project; this thesis evaluates alternate CO2 delivery contracts in terms of incentives offered to the individual entities to make the optimal contingent decisions.

Key findings from this work illustrate that the final project value depends on both the evolution of exogenous risk factors and on the endogenous risks associated with response of the entities to change in the risk factors. The results demonstrate that contractual risk-sharing influences decision-making and thus affects project value. For example, weak risk-sharing such as in fixed price CO2-EOR contracts leads to a high likelihood of sub-optimal decision-making, and the resulting losses can be large enough to affect investment and project continuity decisions. This work aims to inform decision-makers in capital projects of the importance of considering strong contractual risk-sharing structures as part of the risk management process to maximize project value.

Marginal abatement cost (MAC) curves, relationships between tonnes of emissions abated and the CO2 (or greenhouse gas (GHG)) price, have been widely used as pedagogic devices to illustrate simple economic concepts such as the benefits of emissions trading. They have also been used to produce reduced-form models to examine situations where solving the more complex model underlying the MAC is difficult. Some important issues arise in such applications: (1) Are MAC relationships independent of what happens in other regions?, (2) are MACs stable through time regardless of what policies have been implemented in the past?, and (3) can one approximate welfare costs from MACs? This paper explores the basic characteristics of MAC and marginal welfare cost (MWC) curves, deriving them using the MIT Emissions Prediction and Policy Analysis model. We find that, depending on the method used to construct them, MACs are affected by policies abroad. They are also dependent on policies in place in the past and depend on whether they are CO2-only or include all GHGs. Further, we find that MACs are, in general, not closely related to MWCs and therefore should not be used to derive estimates of welfare change. We also show that, as commonly constructed, MACs may be unreliable in replicating results of the parent model when used to simulate GHG policies. This is especially true if the policy simulations differ from the conditions under which the MACs were simulated.

© 2012 Springer

Summary

The US Federal Aviation Administration (FAA) has a goal that one billion gallons of renewable jet fuel is consumed by the US aviation industry each year from 2018. We examine the cost to US airlines of meeting this goal using renewable fuel produced from a Hydroprocessed Esters and Fatty Acids (HEFA) process from renewable oils. Our approach employs an economy-wide model of economic activity and energy systems and a detailed partial equilibrium model of the aviation industry. If soybean oil is used as a feedstock, we find that meeting the aviation biofuel goal in 2020 will require an implicit subsidy to biofuel producers of $2.69 per gallon of renewable jet fuel. If the aviation goal can be met by fuel from oilseed rotation crops grown on otherwise fallow land, the implicit subsidy is $0.35 per gallon of renewable jet fuel. As commercial aviation biofuel consumption represents less than two per cent of total fuel used by this industry, the goal has a small impact on the average price of jet fuel and carbon dioxide emissions. We also find that, as the product slate for HEFA processes includes diesel and jet fuel, there are important interactions between the goal for renewable jet fuel and mandates for ground transportation fuels.

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