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Highlights of Global Climate for 1998

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Highlights of Global Climate for 1998 CLIMATE CHANGE MONITORING REPORT 2007 October 2008 JAPAN METEOROLOGICAL AGENCY Published by the Japan Meteorological Agency 1-3-4 Otemachi, Chiyoda-ku, Tokyo 100-8122, Japan Telephone +81 3 3211 4966 Facsimile +81 3 3211 2032 E-mail [email protected] CLIMATE CHANGE MONITORING REPORT 2007 October 2008 JAPAN METEOROLOGICAL AGENCY Cover: Three-dimensional representations of monthly variations in zonally averaged atmospheric CO2 distribution (concentrations (top) and growth rates (bottom)). This analysis was performed using data archived by the WDCGG. Contents Part I Climate 1 1. Global climate 1.1 Global climate 1 1.2 Global surface temperature and precipitation 4 2. Climate of Japan 2.1 Japan’s Climate in 2007 7 2.2 Major meteorological disasters in Japan 12 2.3 Surface temperature and precipitation in Japan 15 2.4 Long-term trends of extreme events in Japan 17 Column - Long-term trend of heavy rain analyzed from AMeDAS data 24 2.5 Tropical cyclones 27 2.6 The urban heat island effect in metropolitan areas of Japan 29 Part II Oceans 33 1. Global Oceans 1.1 Global sea surface temperature 33 1.2 El Niño and La Niña 35 1.3 Sea ice in the Arctic and Antarctic areas 39 2. The western North Pacific and the seas adjacent to Japan 2.1 Sea surface temperature and ocean currents in the western North Pacific 40 2.2 Sea level around Japan 43 2.3 Sea ice in the Sea of Okhotsk 47 2.4 Marine pollution in the western North Pacific 48 Part III Atmospheric Environment 53 1. Monitoring of greenhouse gases and ozone-depleting substances 1.1 Greenhouse gases and ozone-depleting substances in the atmosphere 54 1.2 Oceanic carbon dioxide 68 1.3 Aerosols 72 2. Monitoring of the ozone layer and ultraviolet radiation 2.1 Ozone layer 76 2.2 Solar UV radiation 81 3. Yellow sand (Aeolian dust) and acid rain 3.1 Yellow sand (Aeolian dust) 84 3.2 Acid rain 86 Map 1 Geographical subdivisions of Japan 88 Map 2 Distribution of surface meteorological observation stations in Japan 89 Part I Climate 1 Global Climate 1.1 Global climate 1.1.1 Major climate anomalies Figures 1.1.1 and 1.1.2 show anomalies in the annual mean temperature (normalized by its standard deviation) and annual total precipitation amount ratios for 2007 respectively. The climatological normal values for temperature and precipitation amounts are calculated using statistics from the period 1971–2000. Figures 1.1.3 and 1.1.4 show frequencies of extremely high/low temperatures and heavy/light precipitation amounts respectively. Extremely high/low temperatures and heavy/light precipitation amounts are defined as values that are observed only once every 30 years or longer. Monthly and seasonal values are omitted in this report. Annual mean temperatures were above normal in most areas of the world except South America (Figure 1.1.1). Extremely high temperatures were frequently observed in East Asia, eastern Siberia and Europe (Figure 1.1.3). Annual precipitation amounts were above normal from Siberia to northern Europe and in Southeast Asia, while they were below normal around the Mediterranean Sea and in northeastern China, the USA and southern Australia (Figure 1.1.2). Extremely heavy precipitation amounts were frequently observed from Siberia to northern Europe and in Southeast Asia, while extremely light precipitation was observed frequently in northeastern China, southern Europe and from southern Australia to New Zealand (Figure 1.1.4). 1.1.2 Extreme climate events Major extreme climate events and weather-related disasters across the world for 2007 are listed below, and are also indicated schematically in Figure 1.1.5. Information regarding disasters is based on EM-DAT (the OFDA/CRED International Disaster Database at the Université Catholique de Louvain in Belgium) and other official reports. (1) High temperatures in eastern Siberia (April–May, August–November) (2) Heavy rains in eastern China (June–July) (3) Tropical cyclone and heavy rains from the Korean Peninsula to China (August) (4) Drought in southern China (September–November) (5) Heavy precipitation in Pakistan (February–March) (6) Tropical cyclone and torrential rains in western Asia (June) (7) Monsoonal torrential rains in India, Nepal and Bangladesh (June–August) (8) Cyclone in Bangladesh (November) (9) High temperatures in western Europe (April) (10) High temperatures in southeastern Europe (May–August) (11) Torrential rains over tropical Africa (July–September) (12) Cold wave in the USA (January–February) (13) Drought in the eastern and western USA (year-round) 1 (14) Drought in northeastern Brazil (year-round) (15) Low temperatures around Argentina (May–August) (16) Drought in southern Australia (July–October) Figure 1.1.1 Annual mean temperature anomalies for 2007 Categories are defined by the annual mean temperature anomaly against the normal divided by its standard deviation and averaged in 5° × 5° grid boxes. The thresholds of each category are -1.28, -0.44, 0, +0.44 and +1.28. Figure 1.1.2 Annual total precipitation amount ratios for 2007 Categories are defined by the annual precipitation ratio to the normal, averaged in 5° × 5° grid boxes. The thresholds of each category are 70%, 100% and 120%. Land areas without graphics represent regions for which observation data are insufficient or normal data are unavailable. 2 Figure 1.1.3 Frequencies of extremely high/low temperatures for 2007 The frequencies of extremely high/low temperatures are marked with upper/lower red/blue semicircles. The size of the semicircle represents the ratio of extremely high/low temperature based on monthly observation for the year in each 5° × 5° grid box. Since the frequency of extremely high/low temperatures is expected to be about 3% on average, occurrence is deemed to be above normal in cases of 10–20% or more. Figure 1.1.4 Frequencies of extremely heavy/light precipitation for 2007 The frequencies of extremely heavy/light precipitation are marked with upper/lower green/orange semicircles. The size of the semicircle represents the ratio of extremely heavy/light precipitation based on monthly observation for the year in each 5° × 5° grid box. Since the frequency of extremely heavy/light precipitation is expected to be about 3% on average, occurrence is deemed to be above normal in cases of 10–20% or more. 3 (1)Warm(1)WarmApr-May, Apr-May, Aug-NovAug-Nov (9)Warm(9)Warm AprApr (10)Warm(10)Warm (5)Wet(5)Wet (2)Heavy(2)Heavy rainrain May-AugMay-Aug (12)Cold(12)Cold wavewave Feb-MarFeb-Mar Jun-JulJun-Jul Jan-FebJan-Feb (6)Cyclone(6)Cyclone (4)Drought(4)Drought JunJun Sep-NovSep-Nov (3)Heavy(3)Heavy rain,rain, TropicalTropical cyclonecyclone AugAug (13)Drought(13)Drought Year-longYear-long (14)Drought(14)Drought Year-longYear-long (7)Heavy(7)Heavy rainrain (8)Cyclone(8)Cyclone Jun-AugJun-Aug NovNov (11)Heavy(11)Heavy rainrain Jul-SepJul-Sep (16)Drought(16)Drought (15)Cold(15)Cold Jul-OctJul-Oct May-AugMay-Aug Figure 1.1.5 Major extreme climate events and weather-related disasters across the world in 2007 1.2 Global surface temperature and precipitation The annual anomaly of the global average surface temperature in 2007 (i.e. the average of the near-surface air temperature over land and the SST) was 0.28°C above normal (based on the 1971–2000 average), and was the sixth highest since 1891 (Figure 1.1.6). The annual mean surface temperature has varied along different time scales ranging from a few years to several decades. On a longer time scale, global average surface temperatures have been rising at a rate of about 0.67°C per century since 1891 (the earliest date for which instrumental temperature records are available). This trend can be explained by global warming caused by the increase in greenhouse gases such as CO2. According to the IPCC Fourth Assessment Report (AR4), most of the observed increase in global average temperatures since the mid-20th century is very likely due to the observed increase in concentrations of anthropogenic greenhouse gases. The surface temperature over the Northern Hemisphere in 2007 was the second highest on record after 2005 since 1891. Surface temperatures over the Northern and Southern Hemispheres have been rising at a rate of about 0.69°C and 0.66°C per century respectively. The ratio of global annual precipitation (for land areas only) to the normal in 2007 (i.e. the 1971–2000 average) was 98%. About 1,200 stations were used to calculate this value. Although no particular trend is seen globally or over the Northern Hemisphere, there has been a remarkable positive trend over the Southern Hemisphere since 1880 (Figure 1.1.7). 4 Figure 1.1.6 Annual anomalies in surface temperature (i.e. the average of the near-surface air temperature over land and the SST) from 1891 to 2007 globally (top), for the Northern Hemisphere (middle) and for the Southern Hemisphere (bottom). Anomalies are deviations from the normal (i.e. the 1971–2000 average). The bars indicate anomalies in surface temperature for each year. The blue lines indicate five-year running means, and the red lines indicate the long-term linear trends. 5 Figure 1.1.7 Annual precipitation ratios (land only) from 1880 to 2007 globally (top), for the Northern Hemisphere (middle) and for the Southern Hemisphere (bottom). The bars indicate the ratios of annual precipitation to the normal (i.e. the 1971–2000 average). The green lines indicate five-year running means. 6 2 Climate of Japan 2.1 Japan’s Climate in 2007 In winter 2006/07 (i.e.
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