Elsevier

Energy

Volume 179, 15 July 2019, Pages 747-761
Energy

The share of cooling electricity in global warming: Estimation of the loop gain for the positive feedback

https://doi.org/10.1016/j.energy.2019.04.170Get rights and content

Highlights

  • Electricity need for cooling buildings in summers is estimated for 12 world regions.

  • Carbon emitted by fossil-fuel power plants for the cooling electricity is estimated.

  • A linear model is used to relate emissions to the land temperature anomaly.

  • Loop-gain is estimated then by multiplying the two estimated coefficients.

  • The positive loop will bring up acceleration again even in optimistic scenarios.

Abstract

Our world's future is strongly connected to energy consumption trends. There are bi-directional relations between energy consumption and the average temperature of Earth, leading to positive causal loops. Increasing temperatures cause activity of more cooling systems most of which are electrified by burning hydrocarbons that consequently yield more carbon dioxide concentration and warmer climates. This paper is a trial to estimate the loop gain by employing a bottom-up regional model. The model is a spreadsheet containing sets of parameters and variables to estimate electricity used for cooling buildings in the residential and commercial sectors of 12 regions all around the world. The share of fossil-fuel based power plants determines each region's contribution to CO2 emissions. Then, by processing data on the global emission trend and land temperature anomaly, a linear ARMAX relationship is estimated to compute the loop gain. The results show that, even in the optimistic scenario of IPCC (A1B), emission from cooling electricity will double up by the end of the century. With the estimated 1 + 1.4 × 10-6 loop gain, even if fossil-fuel electricity generation is gradually reduced to 40%, after a short fall, it will start growing again in the mid-century.

Introduction

Nowadays, nobody can neglect the global warming phenomenon, since most people can sense and see its consequences in all seasons of their life. Climate change acceleration has been a serious concern of researchers for decades [1]. The intergovernmental panel for climate change predicted that the average temperature of our planet will increase by 1.4–5.8 °C by the end of the 21st century [2]. There are researches that propose more pessimistic estimates [3]. The warming speed has been estimated at more than 0.02 °C per year for recent decades. Some researchers estimate the global warming from 1850 conditions to 2080–2100 ranges from 1.5 °C to 4.4 °C under different scenarios [2]. They also address recent acceleration in warming. There exist an extensive literature that discusses the phenomenon by large models, among from System Dynamics (SD) models are of interest [4], used for policy analyses too [5].

The acceleration is probably because of positive feedbacks in the entire carbon concentration system addressed in the literature [3], some of which are represented by Fig. 1. Three main resources of carbon dioxide are supplying the fuel for a long-term dynamics of this system: solar radiation, CO2 emitted by volcanic activities, and the only anthropological one, i.e. fuel burning by human beings. The first loop, denoted by + R1, which accelerates solar radiation absorption, is the effect of temperature rise on the polar ice melting, as well as fewer winter snows cover, which in turn causes expansion of oceans and more darkness of Earth's surface [6]. The second, +R2, is in fact inside the first; even more ocean expansion is in progress because of more waves and storms that eat the shores. Although the oceans act as a giant lung that absorbs CO2, scientists have found that its performance is a function of the atmosphere temperature. Thus, a third positive loop is activated weakening Earth's lungs and reduces both land and ocean uptake of CO2, respectively by 54% and 35%, if the CO2 concentration is four folds [7]. The fourth positive loop has been also warned by scientists several times. The warming atmosphere speeds up the decomposition of belowground organic matter [8]. This also leads to more greenhouse gases (GHG) released into the atmosphere and closes another positive loop, +R4. The next positive loop, +R5, accelerates deforestation, including two other re-enforcing loops that worsen the case by decreasing rainfalls [9].

Before explaining the simple sixth loop, it is worth mentioning how critical is to study the dynamics of these loops. Although many articles have been modeling and analyzing the climate change phenomenon [10], not any paper has quantitatively discussed how exactly these loops affect climate change acceleration. Nonetheless, there are few papers that have estimated one of the individual loop gains, mostly focusing on the third loop. However, wild rapid changes, nonlinearities, and the complicated dynamics have made the researchers to revise and correct their estimates frequently [11].

The Global Carbon Project organization publishes the most recent reports revealing various statistics such as trends for carbon emission (CE) and global warming, as well as predictions of what can happen under different scenarios. The conceptual framework including most of the above-mentioned loops plus some other could be found in reports of the organization which are provided by collaborative efforts of the global carbon cycle science community [12].

Research shows that climate change has an undeniable impact on electricity consumption. The increase of cooling energy demand in Switzerland [13], California [14], and the entire United States [15], studied by researchers, are just a few examples for evidence of such impact. The warmer is going the weather the more electrical energy is needed for cooling and the more fossil fuel is burned for electricity generation. For instance, it is shown by simulation that the peak cooling energy use will increase in the US about 7%–9% in 2020 w.r.t. 1960 [15]. Moreover, the more fuel is consumed for either heating or cooling by electricity, the more important its side effects appear in the climate, i.e. the CO2 emission, global warming, and climate change [16]. This paper aims to analyze one of the factors of the warming acceleration represented by Fig. 2.

On one hand, there are limited resources of energy, mostly fossil fuels. On the other hand, using fossil energy resources for both cooling and heating, with the consequence of CO2 emission, causes the average temperature of Earth to increase [17]. Fig. 2 shows this mechanism in three loops. Energy consumed for cooling emits CO2 that accelerates warming in the middle loop, while in the left side loop, the energy required for heating decreases for the fact that the average temperature has a positive trend. In System Dynamics methodology these are called reinforcing and balancing loops respectively. Apparently, all reinforcing loops exacerbate the problem in the future of the global climate. Focusing solely on the positive trend, other probable positive loops due to colder winters and hotter summers, which are counted as a consequence of meandering phenomenon in jet streams [18], are not shown in these figures and need separate research to conclude their effects.

Hence, researchers ought to think for any solution that adjusts the middle loop with a negative effect and attenuates the corresponding positive gain as much as possible.

Regarding the positive loop, one can make a rough calculation that energy needed for keeping a 100 m2 sample house 1 °C colder than the outdoor temperature for an hour is approximately 0.5 kWh. This energy is mostly provided by electricity, which can be generated by fossil fuels or renewable (clean/carbonless) energies. Both technologies based on cooling by fossil fuel directly, or by fuel-based electric power cause CO2 emission which in turn leads the average temperature of the globe to increase, and so need more energy for cooling. Moreover, other energy demand supplied by fossil fuel, especially in the industrial and transportation sectors, accelerates the warming loop even more. Adding these factors to Fig. 2 in its right-hand loop leads to what is presented by Fig. 3.

Since the energy required for heating is mostly demanded by industries that mainly use fossil fuels, the left-hand side balancing loop is too weak to compensate for the destabilizing effect of the other reinforcing loop. However, if electricity generated by renewable resources is promoted and increased, fossil fuels consumption will reduce, and the warming rate of the global climate will be lowered. Therefore, it seems essential to investigate climatic factors effect on energy consumption in two warm and cold seasons separately.

There are a few studies reporting estimates on the share of cooling electricity in the total electricity consumption all around the world. Although there are accurate engineering methods to calculate the heating/cooling loads, on large-scale, e.g. for a country, it is too difficult to estimate the total worldwide load by such detailed methods. Detailed bottom-up electricity demand estimates are performed for buildings of the European service sector [19], A household energy use breakdown is done in 2009 for the United States [20]. The researchers have found that almost 11% and 14.1% of electricity is consumed for cooling and air-conditioning in these two regions, respectively. Updates can be found for 2014 in Europe [21] and 2015 in the US [22], which refer to 13.7% and 18%, respectively. There are many other works that address how temperature and other climatic variables can impact electricity consumption, both from a technical viewpoint [23,24] or in a macro level for a specific city or country [25,26].

This paper aims to follow up a bottom-up analysis of electricity use in the world and then present a simple method for estimating the loop gain that is comparable with the results obtained by other top-down electricity demand models. An intelligent design of electricity demand model for a sample residential-commercial region [24,25,26,27,28,29,30,31], which includes climatic variables, particularly the temperature, might be used to estimate the total electricity used for cooling. The results are compared with those could be found in the literature to confirm the accuracy of the estimates. Finally, gathering data for the share of fossil-fuel based power plants, the total GHG emissions are calculated and then the global warming acceleration rate caused by cooling the residential-commercial sectors is estimated.

The organization of the paper is as follows. The second section is dedicated to the analysis of electricity demand for space cooling through a bottom-up approximate, yet complicated and efficient model. It is tried to relate almost everything to the temperature. Then the calculation is tracked for a sample region and the results are summarized for 12 regions of the world. In the next section, by using linear approximate models the relationship between GHG emission and the average global temperature anomaly is estimated, where the loop gain is found. A long-term simulation is also designed in two scenarios and the results are compared. Section four concludes the paper.

Section snippets

A regional analysis of electricity demand for space cooling

There are too many works on the estimation of the energy demand of buildings [27]. They utilize various techniques and methodologies [28]. The methods applied for the estimation of buildings cooling/heating energy demands are classified into two main groups: statistical and engineering methods [29]. The engineering methods can be divided to elaborate and simplified methods, based on the availability of data and the accuracy needed. However, there is no apparent boundary to separate the

Emission estimate via an example region: Europe

The above bottom-up calculation is applied for all the 12 regions worldwide, the results of which are given in this section. We are also following the calculations for an example region. Because of more accurate and accessible data Europe region is chosen, to which Russia is augmented, and the specifications for buildings and the environment are assumed as follows:

Solar irradiations are taken from various references such as [[54], [55], [56]]. The average living space is about 105 m2 per

Loop gain and long-term evolution estimates

Evidently, there are complexities and nonlinearities between GHG (carbon dioxide) concentration and the average global temperature referred to by the pioneers [2]. There are very sophisticated almost complete models that can simulate climatic changes [67] or calculate GHG emissions. There are estimates on the total effect of CO2 concentration on the temperature that range from (1.5–4.5) °C for doubled carbon volume in the atmosphere, where no feedback effect is considered [68], to 11.5 °C, if

Conclusion and remarks

There are many causes that are making the globe warmer every year. Many of these causes are positively activating closed loops, known as “snowball effect”, which accelerate the changes over time. Since a complex system is better analyzed and understood if its components are separately analyzed first, one of those positive loops is studied in this research. A bottom-up spread-sheet model is developed to estimate cooling electricity load for 12 regions all around the world. The load is formulated

Acknowledgment

The author is so thankful of the valuable comments of Dr. B. Sajadi, assistant professor at the School of Mechanical Engineering, University of Tehran, as well as the efforts made by H. Zaman, graduate student at Department of Management Sciences and Quantitative Methods, Montreal, Canada, in collection of some parts of data required for the calculations. He is also very thankful for the anonymous reviewers whose valuable comments helped a lot in the improvement of the authenticity of this

References (81)

  • Hamed Shakouri G. et al.

    A novel fuzzy linear regression model based on a non-equality possibility index and optimum uncertainty

    Applied Soft Computing

    (2009)
  • Peter E. Thornton et al.

    An improved algorithm for estimating incident daily solar radiation from measurements of temperature, humidity, and precipitation

    Agricultural & Forestry Meteorology

    (1999)
  • M. Jakubcionis et al.

    Estimation of European Union residential sector space cooling potential

    Energy Policy

    (2017)
  • K. Papakostas et al.

    Heating and cooling degree-hours for Athens and Thessaloniki, Greece

    Renew Energy

    (2005)
  • A. Satman et al.

    Heating and cooling degree-hours for Turkey

    Energy

    (1999)
  • J.F.B. Mitchell et al.

    CO2 and climate: a missing feedback?

    Letters to Nature, Nature

    (1989)
  • National Research Council (NRC)

    Advancing the science of climate change

    (2010)
  • D.A. Stainforth et al.

    Uncertainty in predictions of the climate response to rising levels of greenhouse gases

    Nature

    (2005)
  • Andrew Ford

    System dynamics models of environment, energy and climate change, Encyclopedia of Complexity and applied systems science

    (2009)
  • T. Fiddaman

    Exploring policy options with a behavioral climate-economy model

    Syst Dynam Rev

    (2002)
  • IPCC
    (1996)
  • Pierre Friedlingstein et al.

    Positive feedback between future climate change and the carbon cycle

    Geophysical Research Letters

    (2001)
  • Eric A. Davidson et al.

    Temperature sensitivity of soil carbon decomposition and feedbacks to climate change

    Nature

    (2006)
  • William F. Laurance et al.

    Positive feedbacks among forest fragmentation, drought, and climate change in the Amazon

    Conserv Biol

    (2001)
  • P. Cox et al.

    Acceleration of global warming due to carbon-cycle feedbacks in a coupled climate model

    Nature

    (2000)
  • J.L. Dufresne et al.

    On the magnitude of positive feedback between future climate change and the carbon cycle

    Geophysical Research Letters

    (2002)
  • Global carbon Project

  • Th Franks

    Climate change impacts on building heating and cooling energy demand in Switzerland

    Energy & Buildings

    (2005)
  • Vanek et al.

    Energy systems engineering; evaluation and implementation

    (2012)
  • P. Friedlingstein et al.

    How positive is the feedback between climate change and the carbon cycle?

    Tellus

    (2003)
  • Capua et al.

    Changes in meandering of the northern hemisphere circulation

    Environ Res Lett

    (2016)
  • Tobias Fleiter et al.

    Electricity demand in the European service sector: a detailed bottom-up estimate by sector and by end-use, Improving Energy Efficiency in Commercial Buildings (IEECB) 2010

    (2010)
  • EIA

    Residential energy consumption survey

    (2009)
  • Paolo Zangheri et al.

    Heating and cooling energy demand and loads for building types in different countries of the EU (eERG)

    (2015)
  • EIA

    Residential energy consumption survey

    (2015)
  • Arlan Burdick

    Strategy guideline: accurate heating and cooling load calculations

    (2011)
  • G. Krese et al.

    Analysis of buildings electric energy consumption data using an improved cooling degree-day method

    J. Mechanical Engineering

    (2012)
  • Rébha Ghedamsia et al.

    Modeling and forecasting energy consumption for residential buildings in Algeria using bottom-up approach

    Energy & Buildings

    (2016)
  • Ali Najmi et al.

    Energy consumption in the residential sector: a study on critical factors

    Int. J. Sustainable Energy

    (2016)
  • Longquan Diaoa et al.

    Modeling energy consumption in residential buildings: a bottom-up analysis based on occupant behavior pattern clustering and stochastic simulation

    Energy & Buildings

    (2017)
  • Cited by (13)

    • Evaluation of the thermodynamic analysis of hydrogen production from a middle-temperature intensity solar collector, a case study

      2022, International Journal of Hydrogen Energy
      Citation Excerpt :

      On the other hand, renewable energy-assisted hydrogen production is expected to play a critical role in the forthcoming years. There are three facts of global warming such as volcanic activities, solar radiation, and anthropological emissions [3]. Fig. 1 shows the causes and results of global warming.

    • Cooling supply costs of a university campus

      2022, Energy
      Citation Excerpt :

      Hence, comfort cooling is predicted to increase up to 750% until the year 2050 [7]. The cooling sector is strongly dominated by electric driven technologies, which potentially leads to a doubling of CO2 emissions of the electrical supply for cooling by the end of the century [8,9]. While southern Europe is characterized by high demands for space cooling, Germany has the largest need for process cooling in the EU [10,11].

    • Experimental evaluation of novel photovoltaic/thermal systems using serpentine cooling tubes with different cross-sections of circular, triangular and rectangular

      2020, Energy
      Citation Excerpt :

      Recently, sustainable renewable energies have attracted the researcher’s attention due to fossil fuels’ limitation and also their environmental hazards [1,2].

    View all citing articles on Scopus
    View full text