CLIMATE
CHANGE AND HUMANS
There is a
belief that “culture” and “society” somehow exists in sharp contrast to
“nature” this perspective needs to be discarded (Salvesen, 1992)
. As Shaw (1981) put it,
“Is it not possible that … in a period which intensive agricultural
exploitation was at its lowest ebb, ‘natural’ forces might have taken their
toll of the environment when the artificial restraints of human cultivation were
not at their most effective?” (Shaw, 1981, 11)
. The tribes of central
Germania consisted of agricultural, clan-based hierarchy that would have
certainly been affected by climate change and long sustained drought periods.
According to
geographic determinism, habits and character are molded by physiographic and
environmental conditions. These
conditions are known to have experienced significant changes.
The placement, distribution, occupation, and even habits of humans
respond to climate (Huntington,
1907)
. The philosophy of
geographic determinism has been replaced due to the oversimplification and
stereotypical racial nature of the approach (Huntington, 1907, Lamb, 1977).
However, from a traditional approach to climate-migration studies, these
early approaches are seemingly relevant.
The greatest
barrier to climate-induced migration studies is that strong emphasis on climate
influence over humans instilling notions of powerlessness, as if humans are
helpless and unwitting pawns in nature’s game (Salvesen,
1992)
. Yet, humans have been
greatly affected by climate change in the modern era, especially by prolonged
drought (e.g., the Dust Bowl years and the 1950s drought).
Climate-induced migration does not imply that humans are merely pawns in
nature’s game, but that climate can significantly influence the human
cognitive process. Climate may either synergistically promote or effectively
limit human activity (Salvesen,
1992)
. Some events can easily be
attributed, at least partially, to an amelioration or deterioration of climate (Anderson,
1981)
.
Lucien
Musset suggests that if the climate were consistent then the numbers of the
Germanic invaders in the 3rd century AD would have been considerably
higher than the numbers of Germanic tribes that eventually invaded.
Based upon the estimates of 1st century population
reconstruction and an average growth trend over the next two centuries, there
were far too few invaders coming from Germania into the Roman Empire (Musset,
1975)
. Ellsworth Huntington
(1907) argued a similar concept. He
concluded that the invasions would have been much larger had rainfall been more
consistent during this period, because the population would be expected to
increase if the period were wetter (Huntington, 1907)
. Both of these arguments
are especially interesting in light of the evidence of Germanic tribes moving
inside of Germania in the 2nd century due to increasing populations (Musset,
1975)
.
Something seems to have provoked the Germanic tribes to move within and beyond Germania in the 3rd century. Jordanes (6th century AD) records that the Germans who lived on fertile soil (in the 3rd and 4th centuries AD) were frequently attacked (Jordanes, The Story of the Goths, 22). Does this hold true for the 4th century as well? There are records from Ammianus of the Goths going to war in AD 369 because trade of food products was not allowed (Musset, 1975) . It is necessary to examine the dendrochronological record to determine when periods of sustained drought and non-drought periods occur to see how they relate to the historical record discussed in the previous chapter. The 3rd and 4th centuries AD consist of many sustained drought years, but there are also sustained wet years. Only with the complete examination of the dendroclimatology of the period, is it possible to better understand the movements of the indigenous tribes of Germania.