|Working Group I: The Scientific Basis|
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B. The Observed Changes in the Climate System
Is the Earth’s climate changing? The answer is unequivocally “Yes”.
A suite of observations supports this conclusion and provides insight about the
rapidity of those changes. These data are also the bedrock upon which to construct
the answer to the more difficult question: “Why is it changing?”, which
is addressed in later Sections.
This Section provides an updated summary of the observations that delineate how the climate system has changed in the past. Many of the variables of the climate system have been measured directly, i.e., the “instrumental record”. For example, widespread direct measurements of surface temperature began around the middle of the 19th century. Near global observations of other surface “weather” variables, such as precipitation and winds, have been made for about a hundred years. Sea level measurements have been made for over 100 years in some places, but the network of tide gauges with long records provides only limited global coverage. Upper air observations have been made systematically only since the late 1940s. There are also long records of surface oceanic observations made from ships since the mid-19th century and by dedicated buoys since about the late 1970s. Sub-surface oceanic temperature measurements with near global coverage are now available from the late 1940s. Since the late 1970s, other data from Earth-observation satellites have been used to provide a wide range of global observations of various components of the climate system. In addition, a growing set of palaeoclimatic data, e.g., from trees, corals, sediments, and ice, are giving information about the Earth’s climate of centuries and millennia before the present.
This Section places particular emphasis on current knowledge of past changes in key climate variables: temperature, precipitation and atmospheric moisture, snow cover, extent of land and sea ice, sea level, patterns in atmospheric and oceanic circulation, extreme weather and climate events, and overall features of the climate variability. The concluding part of this Section compares the observed trends in these various climate indicators to see if a collective picture emerges. The degree of this internal consistency is a critical factor in assessing the level of confidence in the current understanding of the climate system.B.1 Observed Changes in Temperature Temperatures in the instrumental record for land and oceans The global average surface temperature has increased by 0.6 ± 0.2°C3 since the late 19th century. It is very likely that the 1990s was the warmest decade and 1998 the warmest year in the instrumental record since 1861 (see Figure 2). The main cause of the increased estimate of global warming of 0.15°C since the SAR is related to the record warmth of the additional six years (1995 to 2000) of data. A secondary reason is related to improved methods of estimating change. The current, slightly larger uncertainty range (±0.2°C, 95% confidence interval) is also more objectively based. Further, the scientific basis for confidence in the estimates of the increase in global temperature since the late 19th century has been strengthened since the SAR. This is due to the improvements derived from several new studies. These include an independent test of the corrections used for time-dependent biases in the sea surface temperature data and new analyses of the effect of urban “heat island” influences on global land-temperature trends. As indicated in Figure 2, most of the increase in global temperature since the late 19th century has occurred in two distinct periods: 1910 to 1945 and since
The regional patterns of the warming that occurred in the early part of the 20th century were different than those that occurred in the latter part. Figure 3 shows the regional patterns of the warming that have occurred over the full 20th century, as well as for three component time periods. The most recent period of warming (1976 to 1999) has been almost global, but the largest increases in temperature have occurred over the mid- and high latitudes of the continents in the Northern Hemisphere. Year-round cooling is evident in the north-western North Atlantic and the central North Pacific Oceans, but the North Atlantic cooling trend has recently reversed. The recent regional patterns of temperature change have been shown to be related, in part, to various phases of atmospheric-oceanic oscillations, such as the North Atlantic-Arctic Oscillation and possibly the Pacific Decadal Oscillation. Therefore, regional temperature trends over a few decades can be strongly influenced by regional variability in the climate system and can depart appreciably from a global average. The 1910 to 1945 warming was initially concentrated in the North Atlantic. By contrast, the period 1946 to 1975 showed significant cooling in the North Atlantic, as well as much of the Northern Hemisphere, and warming in much of the Southern Hemisphere.
New analyses indicate that global ocean heat content has increased significantly since the late 1950s. More than half of the increase in heat content has occurred in the upper 300 m of the ocean, equivalent to a rate of temperature increase in this layer of about 0.04°C/decade.
New analyses of daily maximum and minimum land-surface temperatures for 1950 to 1993 continue to show that this measure of diurnal temperature range is decreasing very widely, although not everywhere. On average, minimum temperatures are increasing at about twice the rate of maximum temperatures (0.2 versus 0.1°C/decade).Temperatures above the surface layer from satellite and weather balloon records Surface, balloon and satellite temperature measurements show that the troposphere and Earth’s surface have warmed and that the stratosphere has cooled. Over the shorter time period for which there have been both satellite and weather balloon data (since 1979), the balloon and satellite records show significantly less lower-tropospheric warming than observed at the surface. Analyses of temperature trends since 1958 for the lowest 8 km of the atmosphere and at the surface are in good agreement, as shown in Figure 4a, with a warming of about 0.1°C per decade. However, since the beginning of the satellite record in 1979, the temperature data from both satellites and weather balloons show a warming in the global middle-to-lower troposphere at a rate of approximately 0.05 ± 0.10°C per decade. The global average surface temperature has increased significantly by 0.15 ± 0.05°C/decade. The difference in the warming rates is statistically significant. By contrast, during the period 1958 to 1978, surface temperature trends were near zero, while trends for the lowest 8 km of the atmosphere were near 0.2°C/decade. About half of the observed difference in warming since 1979 is likely4 to be due to the combination of the differences in spatial coverage of the surface and tropospheric observations and the physical effects of the sequence of volcanic eruptions and a substantial El Niño (see Box 4 for a general description of ENSO) that occurred within this period. The remaining difference is very likely real and not an observing bias. It arises primarily due to differences in the rate of temperature change over the tropical and sub-tropical regions, which were faster in the lowest 8 km of the atmosphere before about 1979, but which have been slower since then. There are no significant differences in warming rates over mid-latitude continental regions in the Northern Hemisphere. In the upper troposphere, no significant global temperature trends have been detected since the early 1960s. In the stratosphere, as shown in Figure 4b, both satellites and balloons show substantial cooling, punctuated by sharp warming episodes of one to two years long that are due to volcanic eruptions.
Surface temperatures during the pre-instrumental period from the proxy record
It is likely that the rate and duration of the warming of the 20th century
is larger than any other time during the last 1,000 years. The 1990s are likely
to have been the warmest decade of the millennium in the Northern Hemisphere,
and 1998 is likely to have been the warmest year. There has been a considerable
advance in understanding of temperature change that occurred over the last millennium,
especially from the synthesis of individual temperature reconstructions. This
new detailed temperature record for the Northern Hemisphere is shown in Figure
5. The data show a relatively warm period associated with the 11th to 14th
centuries and a relatively cool period associated with the 15th to 19th centuries
in the Northern Hemisphere. However, evidence does not support these “Medieval
Warm Period” and “Little Ice Age” periods, respectively, as being globally synchronous.
As Figure 5 indicates, the rate and
duration of warming of the Northern Hemisphere in the 20th century appears to
have been unprecedented during the millennium, and it cannot simply be considered
as a recovery from the “Little Ice Age” of the 15th to 19th centuries. These
analyses are complemented by sensitivity analysis of the spatial representativeness
of available palaeoclimatic data, indicating that the warmth of the recent decade
is outside the 95% confidence interval of temperature uncertainty, even during
the warmest periods of the last millennium. Moreover, several different analyses
have now been completed, each suggesting that the Northern Hemisphere temperatures
of the past decade have been warmer than any other time in the past six to ten
centuries. This is the time-span over which temperatures with annual resolution
can be calculated using hemispheric-wide tree-ring, ice-cores, corals, and other
annually-resolved proxy data. Because less data are available, less is known
about annual averages prior to 1,000 years before the present and for conditions
prevailing in most of the Southern Hemisphere prior to 1861.
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