only 10 and 30 Tg per year respectively (1 Tg =
1 million tons), one-fourth of an early estimate
by other scientists that indicated that rice fields
were not an important source of atmospheric
methane. These findings are significant for the
study of the concentration increase trend of
atmospheric methane, which is an important
greenhouse gas, and for the mitigation option of
methane emission from rice fields.
He has been recognized for his work by receiv-
ing the China National Award for Advances in
Science and Technology and an award for natural
science from the Chinese Academy of Sciences.
Wang has also published many papers and three
important books: Global Warming (1996), Atmo-
spheric Chemistry (1991), and Methane Emission
from Chinese Rice Field (2001). He currently is pro-
fessor of atmospheric chemistry at the Chinese
Academy of Sciences, Institute of Atmospheric
Physics (IAP), Beijing, where he currently is inves-
tigating biogenic (produced by living organisms or
biological processes) emissions in China. The IAP
is China’s highest academic organization in the
basic research of atmospheric sciences, and he has
served as its director from 1997 to 2001.
5 Wegener, Alfred Lothar
(1880–1930)
German
Geophysicist, Meteorologist,
Climatologist
Alfred Wegener was born in Berlin on November
1, 1880, the son of a minister who ran an orphan-
age, and obtained his doctorate in planetary
astronomy in 1904 at the University of Berlin. In
1905, W
egener took a job at the Royal Prussian
Aeronautical Observatory near Berlin, studying
the upper atmosphere with kites and balloons.
Wegener was an expert balloonist, as proved the
following year when he and his brother Kurt set
a world record of 52 hours straight in an interna-
tional balloon contest.
He was invited to go on an expedition to
Greenland as the official meteorologist, from 1906
to August 1908, under the leadership of Ludwig
Mylius Erichsen. The purpose of this “Denmark”
expedition of 28 men was to study polar air circu-
lation and to explore the northeast coast, among
other things. Wegener became the first to use kites
and tethered balloons to study the polar atmo-
sphere. However, Erichsen and two others (Jorgen
Bronland and Hoegh-Hagen) died on the trip.
Ironically, it would be Wegener’s fate more than 25
years later. Returning to Germany in 1909,
Wegener accepted a post as tutor at the University
of Marburg, taking time to visit Greenland again
in 1912–13. He taught at Marburg until 1919.
The idea that continents were connected
was not new. In 1858, Antonio Snider-Pellegrini
suggested that continents were linked during the
Pennsylvanian period some 325 million years ago
because certain Pennsylvanian plant fossils in
Europe and North America were similar. In 1885,
Australian geologist Edward Seuss saw similari-
ties between plant fossils from South America,
India, Australia, Africa, and Antarctica. He
coined the word Gondwanaland for this proposed
a
ncient supercontinent that was made up of these
five landmasses. Finally, in 1910, American
physicist Frank B. Taylor proposed the concept of
continental drift to explain formation of moun-
tain belts in a published paper, but it received no
reaction.
In 1911, Wegener collected his meteorology
lectures and published them as a book, The Ther-
modynamics of the Atmosphere, which became a
standard in Germany and garner
ed Wegener
much acclaim. While at Marburg, he noticed the
close fit between the coastlines of Africa and
South America. His formulation of his theory of
continental drift was the beginning of his search
for paleontological, climatological, and geologi-
cal evidence in support of his theory.
On January 6, 1912, at a meeting of the Geo-
logical Association in Frankfurt, he spoke about
his ideas of “continental displacement” (conti-
Wegener, Alfred Lothar 193