Geography · Ch 17 — World Climate and Climate Change
Climate in the Recent Past
Climate in the Recent Past
Climate is never perfectly stable — it keeps varying, and the recent past gives us plenty of evidence. The twentieth century alone saw dramatic swings: extreme weather, record warmth, and devastating floods and droughts. These events are not random curiosities; they are part of a longer pattern of climate variability that we can trace through historical records.
The 1990s stand out as the warmest decade of the twentieth century, and it also brought some of the worst floods recorded around the world. But the century's climate extremes were not confined to that decade. From 1967 to 1977, the Sahel region — the belt of land just south of the Sahara Desert — suffered a devastating drought that lasted a full decade. Earlier, during the 1930s, severe drought struck the southwestern Great Plains of the United States, an episode so destructive it became known as the Dust Bowl.
How do we know about these changes? Historical records of crop yields and crop failures, accounts of floods, and records of human migration all tell us how changing climate affected people's lives. When harvests failed or lands became uninhabitable, people moved — and those movements are themselves evidence of climate shifts.
Europe's history offers a particularly clear picture of alternating climate phases. The continent repeatedly experienced warm, wet, cold, and dry periods. Two episodes stand out as especially significant:
- Warm and dry conditions in the tenth and eleventh centuries — this was the period when the Vikings settled in Greenland, possible only because the climate was mild enough to support their settlements.
- The "Little Ice Age" from 1550 to about 1850 — a prolonged cooler phase that affected Europe for roughly three centuries. …
The type of climate we experience now might be prevailing over the last 10,000 years with minor and occasionally wide fluctuations. The planet earth has witnessed many variations in climate since the beginning. Geological records show alteration of glacial and inter-glacial periods. The geomorphological features, especially in high altitudes and high latitudes, exhibit traces of advances and retreats of glaciers. The sediment deposits in glacial lakes also reveal the occurrence of warm and cold periods. The rings in the trees provide clues about wet and dry periods. Historical records describe the vagaries in climate. All these evidences indicate that change in climate is a natural and continuous process.
India also witnessed alternate wet and dry periods. Archaeological findings show that the Rajasthan desert experienced wet and cool climate around 8,000 B.C. The period 3,000-1,700 B.C. had higher rainfall. From about 2,000-1,700 B.C., this region was the centre of the Harappan civilisation. Dry conditions accentuated since then.
In the geological past, the earth was warm some 500-300 million years ago, through the Cambrian, Ordovician and Silurian periods. During the Pleistocene epoch, glacial and inter-glacial periods occurred; the last major peak glacial period was about 18,000 years ago. The present inter-glacial period started 10,000 years ago. …