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White
House, June 8 - Vice
President Gore and NOAA scientists announced today that The 1997/98
El Niño, one of the most significant climatic events of
the century, produced extreme weather worldwide. El Niños
have become more frequent and progressively warmer over the past
century, and new data and analysis suggest that global warming
is exacerbating the effects of El Niño. Global temperatures
for January-May 1998 substantially exceed previous records.
During this latest El Niño, temperature and precipitation
records were broken across the United States. Many areas suffered
heavy flooding, and a series of severe tornadoes has killed 122
people so far this year, already matching the annual record set
in 1984. Elsewhere around the world, El Niño contributed
to major droughts and wildfire in Mexico, Indonesia and Brazil;
devastating floods in South America; and massive coral bleaching
from Panama to Africa to Australia's Great Barrier Reef.
Globally, 1997 was the warmest year on record. Average temperatures
for January-May 1998 have since set new all-time highs. Combined
land and ocean temperatures for the five-month period exceed
the previous record by 0.25 C (0.45 F).
Analysis
of data from the ten strongest El Niños of the past century
shows that they are occurring more frequently, and that they
are becoming progressively warmer. These higher temperatures
tend to produce more extreme weather events. Although El Niños
occur cyclically, independent of any long-term warming trend,
there is observational evidence to suggest that rising global
temperatures may be linked to stronger, more frequent El Niños.
THE EL NIÑO PHENOMENON
El
Niño, meaning "Little Boy" or "Christ Child"
in Spanish, was the name given by fishermen to unusually warm
water off the West Coast of South America. El Niños occur
every few years and disrupt the ocean-atmosphere system in the
tropical Pacific, which subsequently affects weather around the
globe. Its far-reaching consequences include increased rainfall
across the southern US and Peru, which has caused destructive
flooding, and drought in the west Pacific, sometimes associated
with devastating fires. During El Niño, the trade winds
which normally blow west towards Indonesia, relax in the central
and western Pacific, allowing normally cool, nutrient-rich waters
off of South America to warm significantly, leading to a decline
in these fisheries. As the Pacific's warmest water spreads eastward,
the hot humid air which fuels thunderstorms moves with it. El
Niño changes the position of the jet stream, winds which
affect the weather not only in North and South America, but as
far away as Africa and Antarctica.
THE
1997/98 EL NIÑO
The
1997-98 El Niño was first noted by numerical models and
scientists at NOAA's Climate Prediction Center in early spring
1997 when sea surface temperatures (SST) in the equatorial Pacific
ocean began to increase. By March 1997, the SSTs were approximately
1 C (1.8 F) above normal in the extreme eastern equatorial Pacific
and the vicinity of the international dateline. By May 1997,
the evolution of the atmospheric and oceanic conditions in the
tropical Pacific were consistent with the beginning stages of
warm episode, or El Niño, conditions. Along with the increased
SSTs, tropical convection began to gradually shift eastward toward
the date line. Numerical models indicated that a continued warming
trend in the tropical Pacific would persist through the end of
the year, and that the warm episode conditions would intensify
during the summer. In May 1997, SSTs greater than 29 C (84 F)
were observed from Indonesia to 160 W. Equatorial SST anomalies
(departures from normal) exceeded +1 C from 175 W eastward to
the South American Coast, with values greater than +4 C (7.2
F) observed in the extreme eastern Pacific. These strong conditions
have persisted in the tropical Pacific Ocean since June 1997.
As of May 1998, strong El Niño conditions continued as
SSTs remained above 28 C throughout most of the region. The latest
NOAA forecasts indicate a return to near normal conditions in
the tropical Pacific during the next 3-6 months. Thereafter,
the NCEP coupled model indicates that near normal conditions
will persist through the end of 1998.
RISING
GLOBAL TEMPERATURES
The most recent near-surface land and
sea-surface ocean temperatures, based on weather stations, ocean
ships and buoys, and satellites indicate that global temperatures
for both land and ocean during 1998 (through May) far exceed
all previous record high temperatures (FIGURE 1). Land temperatures
are 0.32 C (0.58 F) warmer than any previous January-through-May
period. Ocean temperatures are 0.20 C (0.36 F) warmer than any
previous January-through-May period. Combined land and ocean
temperatures exceed the old record by 0.25 C (0.45 F).
The
warmth has clearly been reflected in the US. as temperatures
have averaged 4 to 6 deg F above normal throughout the Great
Lakes States and the Northeast. A number of new one-day record
high temperatures were set during March of this year. They include:
92 F in Connecticut, 95 F in Maryland, 92 F in Massachusetts,
88 F in Vermont, 89 F in Maine, 92 F in New Jersey, and 89 F
in New Hampshire.
The
record warmth is continuing through May as initial data reports
show near-surface land temperatures during May exceeding the
previous record set in 1994 by 0.15 C (0.27 F). Ocean temperatures
also continue to remain at record high levels in May, exceeding
the previous record, set just last year, by 0.15 C (0.27 F).
These record high ocean temperatures are persisting despite some
cooling of ocean temperatures in the Equatorial Pacific related
to the beginning of the demise of the recent El Niño event.
During the
past few decades, global temperatures have persistently broken
previous record highs every few years, but never to the extent
observed in 1998. Each month this year has set a new all-time
record high global temperature (FIGURE 2). This is unprecedented
and is not likely to occur in a stationary climate. New analyses
of tree-rings, historical records, and other proxy measurements
indicate that these temperatures are warmer than the planet has
experienced for at least the last 600 years.
EL
NIÑO AND GLOBAL WARMING
Examination
of data from the ten strongest El Niño events of the Century
reveals two general trends: increasing frequency of El Niño
events in the past few decades, compared to what was observed
earlier this Century; and rising global temperatures during these
events (FIGURE 3). It can not be determined from current evidence
whether El Niños are becoming more frequent or more intense
as a direct result of global warming. It appears evident, however,
that the effects of El Niño could be compounded by rising
global temperatures. In other words, the extreme weather and
climate conditions related to naturally occurring El Niño
events could be exacerbated by an ongoing global warming trend.
The additional heat near the Earth's surface powers the energy
required to evaporate enormous amounts of water. This affects
the entire atmospheric water and energy balance.
El
Niño events also strongly impact regional precipitation
patterns. In the United States, for example, wet conditions ordinarily
occur with El Niño events in the west, south, and southeast.
This year, however, conditions have been wetter than average
throughout virtually the entire country. This continues the Century-long
trend toward wetter conditions in the USA, and more extreme rainfall
and snowfall events.
Based on records dating back
to 1895, many states have broken all-time records for mean temperatures
and total precipitation during the period January-May 1998 (Figure
Map). During the first five months of 1998, records for total
precipitation were broken in California, Maryland, North Carolina,
South Carolina and Virginia. For the same time period, Idaho
had its second wettest year to date, Rhode Island its third wettest,
Nevada its fourth wettest, and Massachusetts, Oregon, and Pennsylvania
their fifth wettest year to date. Outside of California and Arizona
every state has had above average temperatures with 24 states
experiencing much above normal temperatures (in the upper ten
percentile). Thirteen states have had their warmest January -
May period on record. Seventeen states had much above normal
precipitation, nine states had both much above normal precipitation
and temperature, and Maryland had both the wettest and warmest
period on record to date.
While
some regions experience heavy precipitation during El Niño,
in others, increased global temperatures lead to conditions that
are drier than normal. For example, during the past year, Indonesia
and Central America have suffered droughts, which have contributed
to catastrophic wildfires.
APPENDIX: JANUARY-MAY (YEAR-TO-DATE) TEMPERATURE AND PRECIPITATION
RECORDS IN THE CONTIGUOUS UNITED STATES
Many
temperature and precipitation records were broken in the United
States during the January through May period, with several regions
and 17 states setting records for precipitation and temperature
for this period. The Northeast region and 13 states had the warmest
January through May period on record, while the East North Central
and Central regions and the states of Illinois, Indiana, Maine
and Minnesota had the second warmest January through May periods
on record.
During the same period, the Southwest and West regions, and California,
Maryland, North Carolina, South Carolina and Virginia broke records
for precipitation dating back to 1985. Idaho also had the second
wettest five-month period on record.
(Temperatures
in degrees F, Precipitation in inches)
January-May
1998 was the wettest on record (back to 1895) for 2 regions and
5 states:
|
Region |
1998
Value |
1998 Percent
of Normal |
1961-90
Normal |
Second Wettest Value & Year |
|
Southeast |
27.72" |
134% |
20.76" |
27.31 in 1979 |
|
West |
19.66" |
218% |
9.03" |
19.04" in 1995 |
|
|
|
|
|
|
State |
1998
Value |
1998 Percent
of Normal |
1961-90
Normal |
Second Wettest
Value & Year |
|
California |
28.04" |
228% |
12.31" |
27.49" in 1909 |
|
Maryland |
24.55" |
141% |
17.39" |
24.45" in 1924 |
|
North Carolina |
29.20" |
145% |
20.08" |
26.31" in 1979 |
|
South Carolina |
29.98" |
149% |
20.17" |
28.64" in 1929 |
|
Virginia |
27.88" |
162% |
17.26" |
23.30" in 1984 |
January-May 1998 was the second
wettest on record (back to 1895) for 1 state:
|
State |
1998
Value |
1998 Percent
of Normal |
1961-90
Normal |
Wettest
Value & Year |
|
Idaho |
11.89" |
134% |
8.86" |
12.17" in 1996 |
January-May 1998 was the warmest
on record (back to 1895) for 1 region and 13 states:
|
Region |
1998
Value |
1998 Dep.
from Normal |
1961-90
Normal |
Second Wettest
Value & Year |
|
Northeast |
40.9 |
+5.4 |
35.5 |
39.8 in 1921 |
|
State |
1998
Value |
1998 Dep.
from Normal |
1961-90
Normal |
Second Wettest
Value & Year |
|
Connecticut |
43.6 |
+5.2 |
38.4 |
42.8 in 1991 |
|
Delaware |
50.0 |
+4.9 |
45.1 |
49.5 in 1991 |
|
Maryland |
48.8 |
+4.5 |
44.3 |
48.6 in 1990 |
|
Massachusetts |
41.8 |
+4.6 |
37.2 |
41.2 in 1949 |
|
Michigan |
39.1 |
+6.1 |
33.0 |
38.6 in 1921 |
|
|
|
|
|
|
New Hampshire |
37.9 |
+5.2 |
32.7 |
36.1 in 1953 |
|
New Jersey |
47.7 |
+5.4 |
42.3 |
46.4 in 1991 |
|
New York |
40.1 |
+5.8 |
34.3 |
38.9 in 1921 |
|
Ohio |
46.4 |
+5.9 |
40.5 |
45.8 in 1921 |
|
Pennsylvania |
44.5 |
+5.9 |
38.6 |
44.0 in 1921 |
|
|
|
|
|
|
Rhode Island |
44.1 |
+4.5 |
39.6 |
43.0 in 1949 |
|
Vermont |
36.9 |
+5.3 |
31.6 |
35.8 in 1953 |
|
Wisconsin |
38.7 |
+7.2 |
31.5 |
37.9 in 1987 |
January-May 1998 was
the second warmest on record (back to 1895) for 2 regions and
4 states:
|
Region |
1998
Value |
1998 Dep.
from Normal |
1961-90
Normal |
Warmest
Value & Year |
|
East North Central |
38.5 |
+6.4 |
32.1 |
39.0 in 1987 |
|
Central |
48.3 |
+4.4 |
43.9 |
49.0 in 1921 |
|
State |
1998
Value |
1998 Dep.
from Normal |
1961-90
Normal |
Warmest
Value & Year |
|
Illinois |
46.6 |
+5.2 |
41.4 |
47.3 in 1921 |
|
Indiana |
46.7 |
+5.3 |
41.4 |
47.1 in 1921 |
|
Maine |
33.60 |
+4.3 |
29.3 |
33.62 in 1913 |
|
Minnesota |
36.0 |
+7.3 |
28.7 |
37.4 in 1987 |
NOAA/NESDIS/National Climatic
Data Center
Monthly
Climate Highlights || Gore's
Statement
For
additional information contact Pat Viets (301) 457-5005
or Randee
Exler
at (301) 713-0622.
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