EARLY ONLINE RELEASE This is a PDF preprint of the manuscript that has been peer-reviewed and accepted for publication. This pre-publication manuscript may be downloaded, distributed, and cited. Since it has not yet been formatted, copyedited, or proofread, there will be a lot of differences between this version and the final published version. The DOI for this manuscript is DOI:10.2151/jmsj.2015-027 The final manuscript after publication will replace the preliminary version at the above DOI once it is available. 1 2 Comments on "Anthropogenic Heat Release: Estimation 3 of Global Distribution and Possible Climate Effect" by 4 Chen B. et al. 5 6 Fumiaki FUJIBE1 7 8 Meteorological Research Institute, Tsukuba, Japan 9 (Present affiliation: Tokyo Metropolitan University, Hachioji, Japan) 10 11 12 13 May 8, 2015 14 15 16 17 18 19 20 21 22 23 24 -----------------------------------1) Corresponding author: Fumiaki Fujibe, Faculty of Urban Environmental Sciences, Tokyo Metropolitan University, 1-1 Minami-Osawa, Hachioji 192-0397, JAPAN. E-mail: [email protected]. Tel: +81-42-677-2593 Fax: +81-42-677-2589 25 Abstract 26 Chen et al. (2014) estimated the global distribution of anthropogenic heat release 27 (AHR) using satellite observed night lights, and showed a rapid increase of AHR from 28 2000 to 2009 in many regions including Europe and North America. From model 29 simulation based on this estimation, they showed a possibility of substantial influence of 30 AHR on the climate over some regions of the world. However, existing data indicate that 31 neither energy consumption nor night lights changed largely from 2000 to 2009. These 32 facts raise serious doubts about the reliability of their results. 33 34 Keywords: anthropogenic heat release, climate change, night light data 35 2 36 37 1. Introduction 38 Chen et al. (2014; hereafter C14) estimated the global distribution of anthropogenic heat 39 release (AHR) for 1992, 2000, and 2009 using night light data of Defense Meteorological 40 Satellite Program (DMSP)/Operational Linescan System (OLS). Their result indicates that 41 AHR in 2009 was considerably larger than in 2000, possibly by an order of magnitude 42 according to their Figs.2 and 3, reaching an annual mean value of 20Wm-2 in concentrated 43 regions in Europe, North America and East Asia. Using this estimation and a numerical 44 model, they concluded that "AHR has a significant impact on surface temperature and that 45 it is able to affect global atmospheric circulation, leading to a 1-2 K increase in the 46 high-latitude areas of Eurasia and North America". 47 It is believed that AHR can reach 100Wm-2 in the central area of large cities, and has 48 some effects on urban temperature (e.g., Aoyagi et al. 2012). However, area of large AHR 49 is limited, so that contribution of anthropogenic heat to large-scale temperature fields is 50 believed to be negligible, apart from some regions where changes in atmospheric 51 circulation may cause perceivable temperature increase (Zhang et al. 2013). In this respect, 52 the study of C14 may be regarded as presenting a new aspect of the science of global 53 climate. However, there is serious doubt about the validity of their results, as discussed in 54 the following. 55 3 56 57 2. Problems in the AHR estimation by C14 Figure 1 shows the trend of energy consumption in the world and regions provided by the 58 Agency 59 (http://www.enecho.meti.go.jp/about/whitepaper/2014html/2-2-1.html). There is a marked 60 increase in the Asia-Oceania region, which has a number of rapidly developing countries 61 such as China and India, whereas Europe and North America show little change after 2000. 62 In fact, energy consumption in 2009 was of the same amount as that in 2000 in Europe, 63 and 2% smaller than in 2000 in North America. For Japan, the energy consumption in 2009 64 was 65 (http://www.enecho.meti.go.jp/about/whitepaper/2014html/2-1-1.html). for 8% Natural smaller Resources than and Energy that of in Japan 2000 66 Data of DMSP/OLS night light can be obtained from NOAA's National Geophysical Data 67 Center (NGDC). The file of "National trends with intercalibrated DMSP stable light" 68 (http://ngdc.noaa.gov/eog/dmsp/download_national_trend.html) provides annual records of 69 "Sum of Lights (SOL)" in each country since 1992, including "mean SOL" that is an average 70 of SOL from satellites available. Figure 2 shows the trends of mean SOL per unit area for 71 some counties in Europe and East Asia, and USA. It can be seen that SOL does not show a 72 remarkable increase except in China and India. Figure 3 shows the relationship of SOL in 73 2000 and 2009 for each country. The ratio of SOL in 2009 to that in 2000 is 1.79 in China 74 and 1.29 in India, but is less than 1.1 for other countries except Spain (1.14). In fact, the 75 ratio is less than 1 in USA (0.84), UK (0.87), and Japan (0.93). 4 Fig. 1 Fig. 2 Fig. 3 76 Thus both energy consumption and intensity of night lights are found to have changed 77 little from 2000 to 2009 in European countries and USA, and also in Japan. Since C14's 78 estimation of AHR is based on a linear regression of light intensity and anthropogenic heat 79 flux (Fig.1 of Chen and Shi (2012)), AHR should be estimated to be constant as long as 80 SOL is unchanged. We can therefore conclude that the rapid increase of AHR described by 81 C14 is unreliable, and so is their model results based on this estimation as to the influence 82 of AHR on the global climate. 83 84 3. Supplementary remarks 85 Flanner (2009) estimated the global distribution of AHR using energy consumption data. 86 His result for 2005 indicates that "regionally-averaged heat fluxes are sufficiently large (≈1 87 Wm-2)" in western Europe and eastern USA (his Fig.1). In comparison, the values of AHR 88 shown in C14 for 2009 appear to be much larger, seemingly by an order of magnitude 89 according to the coloring of their Fig.3. In other words, the results of Flanner (2009) and 90 C14 are incompatible, apart from the difference of four years. 91 Bennie et al. (2014) analyzed the changes of night light brightness in Europe for 1995 to 92 2010 using the DMSP/OLS data. They showed that "the continental trend is towards 93 increasing brightness", but the rate of increase is not so large (seemingly of the order of 94 10%), while "some economically developed regions show more complex patterns with large 95 areas decreasing in observed brightness". The slight increase of brightness in their analysis 5 96 agrees with the increase of SOL in some countries in Figs. 2 and 3, such as Spain, Italy, 97 and France. 98 99 The results of these studies are consistent with our conclusion that C14's estimation of AHR in 2009 is unrealistically large. 100 101 Acknowledgments 102 The author is grateful to Mr. Takashi Yamada and Mr. Yoshinori Oikawa, JMA, for 103 valuable discussion. 104 105 References 106 Aoyagi, T., N. Kayaba, and N. Seino, 2012: Numerical simulation of the surface air 107 temperature change caused by increases of urban area, anthropogenic heat, and 108 building aspect ratio in the Kanto-Koshin area. J. Meteor. Soc. Japan, 90B, 11-31. 109 Bennie, J., T. W. Davies, J. P. Duffy, R. Inger, and K. J. Gaston, 2014: Contrasting trends in 110 light pollution across Europe based on satellite observed night time lights. Sci. Rep., 4, 111 3789, doi:10.1038/srep03789. 112 113 Chen, B., and G.-Y. Shi, 2012: Estimation of the distribution of global anthropogenic heat flux. Atmos. Oceanic. Sci. Lett., 5, 108-112. 114 Chen, B., L. Dong, G.-Y. Shi, L.-J. Li, and L.-F. Chen, 2014: Anthropogenic heat release: 115 Estimation of global distribution and possible climate effect. J. Meteor. Soc. Japan, 92A, 6 116 117 118 119 120 157-165. Flanner, M. G., 2009: Integrating anthropogenic heat flux with global climate models. Geophys. Res. Lett., 36, L02801, doi:10.1029/2008GL036465. Zhang, G. J., M. Cai, and A. Hu, 2013: Energy consumption and the unexplained winter warming over northern Asia and North America. Nat. Clim. Change, 3, 466-470. 121 122 123 List of Figures Fig.1 Annual energy consumption in the world and regions. Fig.2 Trends of "mean SOL (sum of lights)" per unit area for each country. 124 125 126 127 128 Fig.3 Comparison of mean SOL in 2000 and 2009 for each country. The dashed line is the y=x line. 7 Energy consumption (109 toe) Asia and Oceania Africa Middle East Former USSR Europe C&S America North America Fig.1 Annual energy consumption in the world and regions. SOL (km-2) S. Korea Italy Germany UK Japan France Spain USA India China Fig.2 Trends of "mean SOL (sum of lights)" per unit area for each country. SOL in 2009 (km-2) S. Korea Germany Italy UK France Japan Spain India USA China SOL in 2000 (km-2) Fig.3 Comparison of mean SOL in 2000 and 2009 for each country. The dashed line is the y=x line.
© Copyright 2024