Tree-ring studies suggest that a long wet spell gave him the resources to invade and conquer.
Some
800 years ago, ancestors of modern Mongolians conquered the world on
horseback. A period of unusually mild weather may have helped propel
them by making them rich in livestock.
New research by tree-ring scientists from Columbia University's Lamont-Doherty Earth Observatory
and West Virginia University may have uncovered the reason why an
obscure band of nomadic Mongol horsemen were able to sweep through much
of Asia in a few meteoric decades 800 years ago, conquering everything
in their path: They enjoyed an unprecedented, and yet-to-be-repeated,
15-year run of bountiful rains and mild weather on the normally cold and
arid steppes.
By sampling tree rings in the gnarled and twisted Siberian pines in
the Hangay Mountains in central Mongolia, the team pieced together a
remarkably precise chronology of local climatic conditions stretching
from the year 900 A.D. to the present. The study, published in this week's
Proceedings of the National Academy of Sciences, offers a new interpretation of why the Mongols suddenly went on the move.
To create the climatic chronology, the researchers
sampled tree rings in ancient Siberian pines (like the one above) in the
Hangay Mountains in central Mongolia.
PHOTOGRAPH BY KEVIN KRAJICK/THE EARTH INSTITUTE, COLUMBIA UNIVERSITY
The traditional view has been that the Mongols were desperately
fleeing harsh conditions in their craggy, mountainous homeland. The
Lamont-Doherty team, however, found just the opposite: Between 1211 and
1225—a period that neatly coincides with the rise of Genghis Khan and
the Mongol empire—central Mongolia enjoyed a spell of sustained benign
weather unlike anything the region has experienced during at least the
past 1,100 years and probably much longer.
"What makes our new record distinctive is that we can see 15 straight
years of above-average moisture," says the study's lead author, Neil Pedersen,
a tree-ring scientist with the Lamond-Doherty Earth Observatory. "It
falls during an important period in Mongol history and is singular in
terms of persistently wet conditions."
More Grass, More Horses, More Power
The long run of unusually good conditions meant abundant grasses and a
huge increase in herds of livestock and war horses that became the
basis of Mongol power—a marked contrast to the long and exceptionally
severe droughts that gripped the region during the 1180s and 1190s,
causing unrest and division.
The Mongols saw their opportunity and seized it—and were fortunate
enough that this great tide in their affairs happened to coincide with
the rise to power of a vigorous chieftain who would go on to unite them:
Genghis Khan.
"The transition from extreme drought to extreme moisture strongly
suggests that climate played a role in human events," said tree-ring
scientist Amy Hessl
of West Virginia University in Morgantown, a co-author of the study,
whose research was funded in part by the National Geographic Society's
Committee for Research and Exploration. "It wasn't the only thing, but
it must have created the ideal conditions for a charismatic leader to
emerge out of the chaos, develop an army, and concentrate power. Where
it's arid, unusual moisture creates unusual plant productivity, and that
translates into horsepower—literally. Genghis was able ride that wave."
Tree rings, which can be dated year by year, are clearly visible in well-preserved specimens.
PHOTOGRAPH BY KEVIN KRAJICK/THE EARTH INSTITUTE, COLUMBIA UNIVERSITY
And ride it he did. By the time he died in 1227, he and his followers
had founded an empire that would ultimately cover Korea, China, Russia,
the Middle East, Eastern Europe, Persia, India, and Southeast Asia.
Although the Mongol empire would break up over the centuries, some of
Genghis Khan's direct descendants were still ruling pockets of central
Asia into the 1920s.
The timely change in climatic conditions that helped to
launch the Mongol empire "doesn't appear to have been associated with
any change in volcanic eruptions or solar irradiance," says Kevin Anchukaitis,
a paleo-climatologist at the Woods Hole Oceanographic Institute. The
task that lies ahead: determining if weather influencers like El Niño
and the North Atlantic Oscillation might have brought the beneficial
rains in Central Asia.
High on a landlocked plateau, Mongolia is generally
cold and arid, with tenuous supplies of grass and water. This huge lake
is salty and shrunken from drought.
Mongol Invasion: Modern Version
The climate chronology compiled by the Lamont-Doherty team reveals
that the dawn of the 21st century has seen some of the hottest weather
and most severe droughts in centuries—hotter and drier than even the
severe drought years of the 1180s and 1190s. It also suggests that
climate may play a role in a modern Mongol invasion—from the arid
steppes to the crowded cities.
The recent drought years have followed a string of fairly wet years
toward the end of the 20th century. That's a double whammy, says
Pedersen, since the relative abundance of rainfall in the 1990s could
have made herdsmen less prepared for the harsh conditions of a severe
drought.
The hard years, coupled with sweeping changes in Mongolia's
post-communist society, have sparked a mass exodus from the steppes
into the country's capital, Ulaanbataar, where roughly half of
Mongolia's three-million-strong population now lives.