WMO STATEMENT ON THE STATUS OF THE GLOBAL CLIMATE IN 1995 0.5

0.4

0.3

0.2

0.1

0°C

-0.1

TEMPERATURE ANOMALY -0.2

-0.3

-0.4 World Meteorological Organization -0.5 WMO-No. 838

-0.6 1865 1875 1885 1895 1905 1915 1925 1935 1945 1955 1965 1975 1985 1995 YEAR WMO-No. 838 © 1996, World Meteorological Organization ISBN 92-63-10838-2

Front Cover: 1995 - GLOBALLY, THE WARMEST YEAR ON RECORD World Global land air and sea-surface temperature anomalies (°C) are computed departures from the 1961-1990 base-period Meteorological means. The fitted curve is a 21-point binomial filter. (Source: Hadley Centre, Meteorological Office and Climatic Research Unit, Organization University of East Anglia, United Kingdom) Geneva - Switzerland

Back Cover: Sea-surface temperature anomalies (°C) for December 1994-January 1995 (top) and November 1995 (bottom) computed as departures from the adjusted optimally-interpolated climatology which includes ship observations during the period 1950-1979. (Source: Climate Prediction Center, United States)

Special appreciation is extended to Mr C. Ropelewski, Chairman of the WMO Commission for Climatology Working Group on Climate Change Detection, to other members of the Working Group, and to Mr M. Halpert of the Climate Prediction Center in Washington, D.C., who helped prepare the statement.

NOTE The designations employed and the presentation of material in this publication do not imply the expression of any opinion whatsoever on the part of the Secretariat of the World Meteorological Organization concerning the legal status Printed entirely on of any country, territory, city or area, or of its authorities, or concerning the delimitation of its frontiers or boundaries. recycled paper 3

FOREWORD

There is continuing international concern WMO is responsible for the routine about global warming and its potential to publication of the Climate System Monitoring cause serious disruption to vulnerable social Monthly Bulletin and the biennial Global Climate and economic sectors of society as well as to System Reviews, which are outputs from the sustainable development efforts. As recently Climate System Monitoring Project of the as December 1995, scientists of the World World Climate Data and Monitoring Meteorological Organization/United Nations Programme (WCDMP). Beginning in 1993, Environment Programme (WMO/UNEP) WMO, in its role as a provider of credible Intergovernmental Panel on Climate Change scientific information on climate and its varia- stated that “the balance of evidence suggests bility, began issuing statements on the status a discernible human influence on global of the global climate. This booklet, the third climate”, through emissions of greenhouse in the series, focuses on the status of global gases. At the same time, there is a develop- climate during 1995, and is provided through ing capability within national Meteorological the Climate Change Detection Project of the and Hydrological Services (NMHSs) to WCDMP. provide comprehensive information on past, This statement is a summary of the present, and future (seasons to a year ahead) information provided by the Climate climate and its variations, to a wide spectrum Prediction Center (CPC) in the United States of users. The rapid development of global with inputs from climate centres in communications systems means that such Australia, Canada, Germany, Iceland, information can be provided on a timely basis Netherlands, Russian Federation, Spain, and is, therefore, of great use to national and the United Kingdom. The contributions decision makers. were based, to a great extent, on the obser- Much of our knowledge on climate vational data collected and disseminated on comes from global scientific and technical a continuing basis by the NMHSs of the programmes coordinated by WMO. WMO Member countries.

(G. O. P. Obasi) Secretary-General 4

SUMMARY

The 1995 estimated global mean surface stratosphere was once again almost totally temperature over land and marine areas was destroyed. Carbon dioxide and methane the warmest since 1861. The warmth could concentrations in the atmosphere increased not be attributed to El Niño/Southern in 1995 at their recent historical rates Oscillation (ENSO) since the contrasting following a slow-down in rates of increase in equatorial Pacific Ocean surface temperature 1992 and 1993. anomalies were averaged to be near normal There were many extreme climatic for the year. In the North Atlantic, however, anomalies and weather events in 1995. The sea-surface temperatures were more than most active hurricane season in the Atlantic 1°C warmer in an area centred on the Azores. Ocean since 1933 caused considerable Parts of Siberia averaged more than 3°C property damage in the Caribbean islands warmer than the 1961-1990 period and many and the south-east coastal areas of the heat-related deaths occurred in both the United States. Following prodigious rains in midwest United States and India during the January and February, which caused massive northern hemisphere summer. As is usual, flooding along major continental European there were regions where the temperatures rivers, the summer over the same region were cooler than normal in 1995, including was of near record heat and, in the United Greenland and the adjacent north-west Kingdom particularly, serious precipitation Atlantic Ocean as well as mid-latitudes of deficiencies caused widespread restrictions the North Pacific Ocean. on water usage. There were examples of With respect to atmospheric consti- beneficial events, including the return of tuents, the ozone hole, which has become a abundant rains to such widely separated but feature of the Antarctic spring period, began drought-stricken regions as north-west earlier and lasted longer than in any previ- Africa/Iberian Peninsula, southern Africa, ous recorded year - ozone in the lower and Australia. 5

THE WARMEST YEAR SO FAR

The globally-averaged surface temperature early 1995. A narrow band of the eastern for 1995 was 0.40°C above the 1961-1990 equatorial Pacific is now cooler, indicating a average, according to observations made at weak cold episode (La Niña) condition and land stations along with sea-surface temper- suggesting that, on a global average, 1996 may atures measured from ships and buoys. The be slightly cooler than 1995 (see back cover). previous warmest year since 1861 was 1990, In 1995, the northern hemisphere was which had an anomaly of 0.36°C for the year warmer than in all previous years, but the as a whole (see front cover). southern hemisphere was relatively less warm. Global surface temperatures have now Parts of Siberia were about 3°C warmer than completely recovered from the cooling usual in 1995, because the early part of the year effects associated with the June 1991 erup- was exceptionally warm, whereas 1995 was tion of Mount Pinatubo in the Philippines. A slightly cooler than normal over the Greenland/ prolonged period of the El Niño/Southern north-west North Atlantic region and over the Oscillation (ENSO) warm episode, which mid-latitude North Pacific. It was the coldest dominated the 1991-1994 period, ended in year in Iceland since 1983. These features (see

90N FIGURE 1. Surface temperature anomalies (°C) for January- December 1995. The 45N analysis is based on at least eight months of data for each grid square. Areas with insufficient data are 0 blank. Anomalies are departures from the 1961- 1990 base-period means. (Source: Hadley Centre, 45S Meteorological Office and Climatic Research Unit, University of East Anglia, United Kingdom)

90S 180 120W 60W 0 60E 120E 180 -1 0 1 2 3 4 6

Figure 1) have recurred in many recent years. PROLONGED ENSO WARMING ENDS Also in 1995, the ocean surface was more than 1°C warmer than usual near the Azores. The ENSO warm episode conditions domi- Warm conditions characterized much of nated the tropical Pacific during the period western Europe, reaching record or near from 1990 to early 1995. Thereafter, equatorial record annual means. For instance, in the central and eastern Pacific Ocean surface Netherlands, the mean, spatially-averaged temperature anomalies steadily decreased, temperature for 1995 reached 10.4°C, more becoming negative during the latter half of than 1°C higher than the 1901-1987 average. 1995, as weak cold episode conditions devel- Intense heat, along with high humidity, was a oped in the region. For the first time since feature in July over large areas of the central 1989, equatorial Pacific Ocean surface and eastern United States, and extending into temperatures were below normal throughout central Canada where it was accompanied by the region from the International Date Line severe forest fires. There were over 1 000 eastward to South America. Negative sea- deaths related to the heat. Very high tempera- surface temperature anomalies also spread tures were also prevalent in northern India both north and south from the Equator, so during much of June with temperatures aver- that by the end of 1995 a rather broad band aging up to 5°C above normal, maximum of negative anomalies covered the region (see temperatures reaching 50°C and night-time back cover). Consistent with the reversal in temperatures failing to fall below 25-30°C. the sign of ocean surface temperature anom- Cooling in the lower stratosphere stabi- alies, cloudiness and rainfall decreased to lized in 1995 (see Figure 2) with anomalies less than normal over the central equatorial remaining near the lowest values observed in Pacific and increased to greater than normal the 17-year satellite-measured record. over Indonesia.

1.5 FIGURE 2. Global mean 1.2 lower stratospheric 0.9 temperature anomalies 0.6 (°C) from the Microwave Sounding Unit channel 4. 0.3 The two sharp peaks were ° 0 C associated with the major -0.3 volcanic eruptions of El -0.6 Chichón (March, 1982) and Mount Pinatubo

TEMPERATURE ANOMALY -0.9 (June, 1991). The base -1.2 period is for 1982-1991. -1.5 (Data provided by the University 1980 1982 1984 1986 1988 1990 1992 1994 YEAR of Alabama at Huntsville) 7

LONGEST ANTARCTIC OZONE mid-September to October showed near HOLE DURATION ON RECORD complete destruction of the ozone at alti- tudes between 14 and 21 km. The area of the Ozone measurements during the winter- ozone hole exceeded 22 million km2 and spring of 1994/1995 indicated that total was similar to the recent record set in 1993 column ozone was unusually low over most (see Figure 3). In 1995, however, the dura- of the northern hemisphere. For middle and tion of the time with lower ozone values was high latitudes, ozone values were an longer than ever previously documented. unprecedented 10-20 per cent lower than the average values observed during the CARBON DIOXIDE AND 1957-1980 period. METHANE INCREASE Over Antarctica, ozone depletion began earlier in August than previously and, Provisional indications show that atmos- by late September and for the whole pheric concentrations of both carbon FIGURE 3. Vertical ozone month of October, the deficiency was more dioxide and methane, two principal green- profiles from balloon sound- than 50 per cent, which was comparable to house gases, increased in 1995 at rates ings at the South Pole on that observed over the previous six years. which are in line with their recent historical 23 August 1993 (close to Ozone soundings from a number of trend. It is recalled that these gases exhib- normal values) and on two Antarctic stations during the period from ited a noticeable slow-down in their rates of typical days in October increase during 1992 and 1993 for reasons (1993 and 1995) when that are not presently understood. The total ozone was severely atmospheric concentration of carbon diox- depleted. October 1993 ide now stands at about 360 parts per showed the highest level of million volume (ppmv) compared to an esti- ozone destruction on record. mated 280 ppmv before the start of This illustrates the complete widespread industrialization around 1850. ozone destruction in the lower stratosphere (in these SNOW COVER OVER THE cases between 14 and NORTHERN HEMISPHERE 21 km). This feature was observed at all Antarctic The last five months of 1995 showed positive stations, especially during snow cover anomalies over the northern the second half of September hemisphere. This was the first time since 1984 and throughout October that positive global snow cover area anom- during the “ozone hole” alies were observed for each of these early events of the past seven months of the upcoming snow season. A years. predominance of negative snow cover anom- (Source: Climate Prediction alies early in the year resulted in a 1995 Center, United States) annual mean of 24.5 x 106 km2, only slightly 8 less than the 1973-1995 yearly average. The Central African Republic coincidence of near-average snow cover area Photo: H. Fromm with near-record land surface temperatures is in marked contrast to the record warm year of 1990, which had the least snow cover in the satellite record.

REGIONALLY SPEAKING… Abnormal precipitation in Dryness in Africa and the central South America Mediterranean Persistent below normal precipitation Significant below normal precipitation anom- occured over parts of South America in early alies during 1995 were recorded in both May and continued into mid-December. north-west and southern Africa, which Large sections of central and southern extended to both the western Mediterranean Brazil, southern Paraguay, and central and and the Middle East. In the north-west, well north-eastern Argentina received less than below normal rainfall was recorded across the 75 per cent of normal precipitation during region during the periods from January to the period 1 May-19 December, with less early February, and from late March to May, than 50 per cent of normal totals recorded adding to long-term moisture deficits in parts of the northern state of Rio Grande throughout much of Morocco, Algeria, and do Sul in Brazil, south-eastern Paraguay, Tunisia that had started in November 1994. and the Argentine provinces of Corrientes, Less than 50 per cent of normal precipitation northern Santa Fe, and a few other areas was measured from 1 November 1994 to along the western tier of the region. Forest 25 June 1995 across northern and western fires, the worst in living memory, broke out Morocco, central Tunisia, much of central and in some areas of Argentina. In late north-eastern Algeria, and the Iberian December, however, torrential rains (467 mm Peninsula and southern France. Long-term on 24-25 December) fell along the coast of shortages remained until surplus November the state of Santa Catarina in southern and December precipitation fell over most of Brazil, and heavy showers (100 to 250 mm the region. on 24-30 December) were recorded in much In southern Africa, the 1994-1995 wet of the states of Paraná, Minas Gerais, Rio de season (October-April) was slow to com- Janeiro, and São Paulo. Locally, severe mence across much of Botswana and flooding affected Santa Catarina and Minas northern and central South Africa. Dry condi- Gerais, according to Brazilian authorities. tions spread across most of the region in 9

FIGURE 4. Seasonal The “big dry” ends in Australia satellite-derived rainfall estimates in mm per The ENSO event that had plagued most of month. Anomalies are eastern and southern Australia with drought departures from the 1986- during 1994 slowly diminished through 1993 base-period means. 1995. By the middle of 1995, most tropical (Source: Climate Prediction Pacific indicators showed the termination of Center, United States) the ENSO conditions. Towards the end of 1995, these same indicators suggested the development of a La Niña event. As the ENSO declined, rainfall across Australia returned to normal (see Figure 4), and often above normal levels, breaking the drought in many areas. However, this transition from drought was neither abrupt nor uniform, with dry conditions lingering in some areas until well into the year. January saw the first signs of a break from the dry conditions. The period from February to April saw a return to drier than normal conditions across most of eastern Australia, although April was wet over the far south-east and most of west- ern Australia (except the south-west). The period from May to July was particularly wet over eastern South Australia, Victoria, and November, with near normal rain confined to south-west New South Wales - totals for north-west and south-west Botswana. June and July were among the highest on Subnormal monthly totals, however, were record, and flooding became a regular occur- again reported over much of central and rence. By the end of July, these rains had north-central South Africa and western removed most long-term deficiencies (as Botswana, despite significant December rains measured from April 1994) from south-eastern in some north and eastern areas of the Australia. August stood out as an exception- region. As a result, long-term moisture short- ally mild and dry month over most of extra- ages covered much of southern Africa as 1995 tropical Australia - across large areas it was began. Although occasional significant rains both the warmest and driest August on record. drenched parts of the area up to the end of Coinciding with the onset of La Niña-like April, for the 1994-1995 wet season as a conditions over the Pacific Basin, the period whole, subnormal rains were the general rule from September onwards saw a trend toward over the vast majority of the region. distinctly wetter than normal conditions 10 3.0 across north-eastern South Australia, most of New South Wales, and Queensland. Wet 2.0 conditions were particularly marked in November, when large areas received abun- 1.0 dant rainfall, with local record-breaking precipitation and significant flooding in south- ° ern Queensland, and parts of southern Victoria 0 C during both October and November, although western Victoria and southern South Australia -1.0 had a dry spring. In the tropics, active convec- TEMPERATURE ANOMALY tion produced an early start to the wet season. -2.0 Abnormal conditions from the -3.0 1890 1900 1910 1920 1930 1940 1950 1960 1970 1980 1990 2000 British Isles to central Asia YEAR The main feature of 1995 over the region was Abnormal warmth was evident during the last FIGURE 5. Annual abnormal warmth. In central England, four months of 1995 in most of the region. surface temperature however, 1995, as a whole, was not as warm Central Europe began the year with anomalies for the former as 1990 or 1949 due to a cold month of abundant rainfall and rapidly melting snow, Soviet Union. The red December. Taken together, July and August, which caused flooding and widespread curve is an 11-year were the warmest ever in the record for damage along major rivers, especially in the running mean. central England since 1659. Temperatures Netherlands. Anomalies are departures reached 34°C in some places and 30°C was from the 1951-1980 base- even reached in northern Scotland. Combined A very active period means. with this record summer warmth was extreme season (Source: Institute for Global dryness. Rainfall over the summer in England Climate and Ecology, Russia) and Wales was similar to that experienced in The 1995 Atlantic hurricane season featured 19 1976, which was the driest in the series since tropical storms, 11 of which became hurri- 1766. Spain also experienced hot, dry weather canes. This was the second largest number of with temperatures soaring to a record 47°C at storms (21 in 1933) observed in any hurricane Seville and Cordoba in July. season since records began in 1871, and the Russia and adjacent central Asia mean- second greatest number of hurricanes (12 in while generally experienced their warmest 1969) in one season since hurricane statistics year on record in 1995 (see Figure 5). Weekly began in 1886. The season started early as temperatures of 15°C above normal were became the first June hurri- common north of the Arctic Circle from mid- cane since Bonnie in 1986. August was a busy February to the end of April. In early July, month with dumping 100 to temperatures soared to 47°C in parts of 250 mm of rain over central and extreme north- Turkmenistan and the Republic of Kazakhstan. western . In mid-August, 11

stalled offshore 240 km east of Cape Hatteras, the second hurricane to strike the western North Carolina lashing much of the East Coast Florida Panhandle since early August. Torrential with rough surf and beach erosion. Hurricane rains (300 to 430 mm), a five- to six-metre storm Luis raked the north-eastern Caribbean with surge, and winds gusting to 230 km/h buffeted destructive winds (gusts up to 235 km/h on the western Florida Panhandle and adjacent Antigua before the anemometer blew away) Alabama. Hurricane-force (121 km/h) winds pene- and heavy rains (up to 210 mm in Puerto Rico). trated as far inland as Atlanta, causing , a particularly compact hurri- considerable property damage and disrupting cane, caused extensive damage on the islands electrical power in many areas from the central of St. Croix, Culebra, and St. Thomas. Winds Gulf Coast north-eastward to the Carolinas. were clocked to 200 km/h in St. Croix. In early Farther south, buffeted the October, became the fourth Yucatán Peninsula and . At Cancún, tropical system to affect Florida in 1995, and 400 mm of rain accompanied this hurricane.

SignificantJ climate anomalies and events during 1995

Brief but deadly July Wet & stormy Jan.-May; Mild most of the year ° heat wave (41 C) Chicago, IL; Scandinavia flooding annual temps. 2 - 4˚C above normal warm summer Dry hot summer Apr.-May (north & east sections) Drought Jun.-Sep., Heavy rains & Heavy rains then heavy Surplus precipitation flooding May.-Aug.; Oct. precip. second half of year Very mild Apr.-May Dem. People’s Rep. Korea Apr.-May & Sep. Driest England floods (Aug.) Subnormal 1994-1995 and Wales summer Severe flooding June heat wave wet season; heavy in three centuries Jan.-Feb. temps. to 50˚C Dry Aug.-Dec. rains/flooding Nov.-Dec. Protracted drought Periodic typhoons, Very wet summer & Severe Jan. & Warm Apr.-May heavy rains & early fall (up to 1 525 mm Mar. floods; OPAL & Oct.-Dec. severe flooding dry start to of rain in four months) Torrential Sub-normal rainfall (up to 4 225 mm 1995-1996 rains in July [190% nomal] Jun.-Dec.) wet season Luis & Marilyn Near normal Dry Jan.-May hit northern rainy season Active & Oct.-Dec. Hurricanes Opal Leewards (Sep.) monsoon Super-typhoon Angela & Roxanne hit Surplus monsoon devastates Luzon (Nov.) within 10 days, Sep./Oct. Second most active rains (seventh wettest hurricane season Jul.-Sep. since 1918) since records El Niño ends early; Surplus rains Cyclone Bobby (Feb.) began in 1871 Subnormal weak cold episode (19 named storms) & localized flooding Jan.-Apr. & Oct.-Nov. 1994-95 wet (La Niña) season Brief severe flooding Mild winter in Buenos Aires (Apr.) Drought Severe late Dec. Bobby drops eases Severe floods 45-65% of winter Subnormal Drought annual normal Apr. - Dec. rains Oct. 94-Apr. 95; precipitation Wet Jan.-Feb. wet Nov. & Dec. within a few days after slow start to Lowest N.Z. temp. ever 1995-1996 wet season (-21.6 °C at Ophir Jul.)

Source: Climate Prediction Center, United States December 1994-January 1995 30N

20N

10N

EQ

10S

20S

30S 100E 120E 140E 160E 180 160W 140W 120W 100W 80W -3 -2.5 -2 -1.5 -1 -0.5 0.5 1 1.5 2 2.5 3

November 1995 30N

20N

10N

EQ

10S

20S

30S 100E 120E 140E 160E 180 160W 140W 120W 100W 80W -3 -2.5 -2 -1.5 -1 -0.5 0.5 1 1.5 2 2.5 3