Robert Kar
Thu, Jan-04-07, 17:17
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Collapse of civilisations linked to monsoon changes
a.. 11:13 04 January 2007=20
b.. NewScientist.com news service=20
c.. Catherine Brahic=20 The downfall of the one of the
greatest Chinese dynasties may have been = catalysed by
severe changes in climate. The same climate changes may =
have simultaneously led to the end of the Maya
civilisation depicted in = Mel Gibson's new film
Apocalypto.=20
So says Gerald Haug of the GeoForschungsZentrum in Germany and
= colleagues, who studied geological records of monsoons over
the past = 16,000 years. They have found a startling
correlation between climate = extremes and the fall of two
great civilisations: the Tang dynasty in = China and the Maya
of South America. "It blew me away," says Haug.
The records show that around the time that these civilizations
went into = decline, they experienced stronger than average
winds in the winter and = weaker summer monsoon rains. These
weak rains would have reduced crop = yields.
Records of monsoons beyond the last 50 years are difficult to
obtain. = Looking for signs of monsoon trends in geological
records going back = thousands of years can help solve this
problem. In China, stalagmites = provide the best available
historical record of summer monsoon rains, = says Haug, as
more rain increases the amount of water dripping down from =
the roofs of caves. But until now, there has been no reliable
estimate = of winter winds.=20
Iron and titanium Haug and his colleagues solved this problem
by studying the sediments = deposited at the bottom of Lake
Hugauang Maar in southeastern China. The = sediments are made
up primarily of material deposited there by winter = monsoon
winds because the catchment area is small, meaning very few =
streams bring in sediments from other sources. As a result,
the = sediments provide an accurate historical record of the
strength of the = winter monsoon winds.
The researchers looked at iron and titanium levels in a
sediment core = that was extracted from the lake floor. The
oxidation level of the iron = told them how much oxygen was
present in the lake waters when the = sediments were
deposited, and therefore how much wind was stirring up = the
lake surface. Titanium in particles is non-reactive and the =
quantities accumulated in the layers of sediment provided
another = measure of wind strength.
When they compared the 16,000 years represented by the mud
core, the = researchers found that years of strong winter
winds corresponded very = closely to strong summer rains and
vice versa. "Our sediment data = provides a mirror image to
summer records in stalagmites," explains = Haug.=20
The researchers believe the only coherent explanation for the
summer and = winter trends and is a shift in the position of a
band of low-pressure = that girdles the Earth, known as the
inter-tropical convergence zone, or = ITCZ.=20
They found that when warm temperatures in the Northern
hemisphere = indicated a northward shift of the ITCZ, summer
monsoon rains were = strong and winter monsoon winds were
weak. "It seems possible that major = shifts in ITCZ catalysed
simultaneous events in civilisations on = opposite sides of
the Pacific Ocean," conclude the researchers in a = paper in
Nature.=20
Catalysing effect Previously, Haug had shown that the
repetitive periods of decline of the = Mayan civilisation in
Latin America corresponded to dry periods on that =
continent.=20
The Maya civilisation and Tang dynasty were contemporary and
there is a = striking similarity between the Chinese and Latin
American climate data. = These include a general shift towards
a drier climate around AD 750 and = three very dry periods
between then and AD 910, the last of which = coincides with
both the Maya and the Tang collapse.
"I am not a historian," cautions Haug, but "there is a
coincidence at = least". He says his work is part of "a
growing piece of evidence that = climate has catalysing effect
on societies".
Analysing historical monsoon records can be extremely useful
in making = future climate predictions. For instance, some
researchers suggest that = strong summer monsoon rains are
preceded by weak winter winds. If true, = this theory could
prove extremely useful in preparing agriculture for a =
difficult year ahead.=20
Journal reference: Nature (vol 445, p 74)
Source: NewScientist http://environment.newscientist.com/arti-
cle/dn10884?DCMP=3DNLC-nletter&ns= ref=3Ddn10884
--=20 Posted by Robert Karl Stonjek
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<STYLE></STYLE> </HEAD> <BODY> <DIV id=3DartHeadline> <H1
class=3Dinline><FONT size=3D5>Collapse of civilisations linked
to = monsoon=20 changes</FONT></H1></DIV> <UL class=3D"notlist
highlight" id=3Dartdetails>
<LI>11:13 04 January 2007=20
<LII>NewScientist.com news service=20
<LII><A>Catherine Brahic</B> </LI></UL>
<DIV>
<DIW>The downfall of the one of the greatest Chinese
dynasties may have = been=20 catalysed by severe changes
in climate. The same climate changes may = have=20
simultaneously led to the end of the Maya civilisation
depicted in Mel = Gibson's=20 new film
<I>Apocalypto</I>. </P>
<DIX>So says Gerald Haug of the GeoForschungsZentrum in
Germany and = colleagues,=20 who studied geological
records of monsoons over the past 16,000 years. = They
have=20 found a startling correlation between climate
extremes and the fall of = two great=20 civilisations:
the Tang dynasty in China and the Maya of South
America. =
=93It blew=20
me away," says Haug.</P>
<DIY>The records show that around the time that these
civilizations went = into=20 decline, they experienced
stronger than average winds in the winter and = weaker=20
summer monsoon rains. These weak rains would have reduced
crop = yields.</P>
<DIZ>Records of monsoons beyond the last 50 years are
difficult to obtain. = Looking=20 for signs of monsoon
trends in geological records going back thousands = of
years=20 can help solve this problem. In China,
stalagmites provide the best = available=20 historical
record of summer monsoon rains, says Haug, as more rain =
increases the=20 amount of water dripping down from the
roofs of caves. But until now, = there has=20 been no
reliable estimate of winter winds. </P>
<DIZ1><FONT size=3D4>Iron and titanium</FONT></H5>
<DIZ>Haug and his colleagues solved this problem by studying
the sediments =
deposited at the bottom of Lake Hugauang Maar in southeastern
China. The =
sediments are made up primarily of material deposited there by
winter = monsoon=20 winds because the catchment area is small,
meaning very few streams = bring in=20 sediments from other
sources. As a result, the sediments provide an = accurate=20
historical record of the strength of the winter monsoon
winds.</P>
<DIZ>The researchers looked at iron and titanium levels in a
sediment core = that=20 was extracted from the lake
floor. The oxidation level of the iron told = them how=20
much oxygen was present in the lake waters when the
sediments were = deposited,=20 and therefore how much
wind was stirring up the lake surface. Titanium = in=20
particles is non-reactive and the quantities accumulated
in the layers = of=20 sediment provided another measure
of wind strength.</P>
<DIZ>When they compared the 16,000 years represented by the
mud core, the=20 researchers found that years of strong
winter winds corresponded very = closely to=20 strong
summer rains and vice versa. "Our sediment data provides
a mirror = image=20 to summer records in stalagmites,"
explains Haug. </P>
<DIZ>The researchers believe the only coherent explanation for
the summer = and=20 winter trends and is a shift in the
position of a band of low-pressure = that=20 girdles the
Earth, known as the inter-tropical convergence zone, or =
ITCZ. </P>
<DIZ>They found that when warm temperatures in the Northern
hemisphere = indicated a=20 northward shift of the ITCZ,
summer monsoon rains were strong and winter = monsoon=20
winds were weak. "It seems possible that major shifts in
ITCZ catalysed=20 simultaneous events in civilisations on
opposite sides of the Pacific = Ocean,"=20 conclude the
researchers in a paper in <I>Nature</I>. </P>
<DIZ1><FONT size=3D4>Catalysing effect</FONT></H5>
<DIZ>Previously, Haug had shown that the repetitive periods of
decline of = the=20 Mayan civilisation in Latin America
corresponded to dry periods on that=20 continent. </P>
<DIZ>The Maya civilisation and Tang dynasty were contemporary
and there is = a=20 striking similarity between the
Chinese and Latin American climate data. = These=20
include a general shift towards a drier climate around AD
750 and three = very dry=20 periods between then and AD
910, the last of which coincides with both = the Maya=20
and the Tang collapse.</P>
<DIZ>"I am not a historian," cautions Haug, but "there is a
coincidence at = least".=20 He says his work is part of
"a growing piece of evidence that climate = has=20
catalysing effect on societies".</P>
<DIZ>Analysing historical monsoon records can be extremely
useful in = making future=20 climate predictions. For
instance, some researchers suggest that strong =
summer=20 monsoon rains are preceded by weak winter
winds. If true, this theory = could=20 prove extremely
useful in preparing agriculture for a difficult year =
ahead. </P>
<DIZ>Journal reference: <I>Nature</I> (vol 445, p 74)</P>
<DIZ>Source: NewScientist<BR><A=20 href=3D"http://environment-
.newscientist.com/article/dn10884?DCMP=3DNLC-nl= etter&a-
mp;nsref=3Ddn10884">http://environment.newscientist.com/-
article/dn=
10884?DCMP=3DNLC-nletter&nsref=3Ddn10884</A></P>
<DIZ><BR>-- <BR>Posted by<BR>Robert Karl
Stonjek</P></DIV></BODY></HTML>
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quoted-printable
Collapse of civilisations linked to monsoon changes
a.. 11:13 04 January 2007=20
b.. NewScientist.com news service=20
c.. Catherine Brahic=20 The downfall of the one of the
greatest Chinese dynasties may have been = catalysed by
severe changes in climate. The same climate changes may =
have simultaneously led to the end of the Maya
civilisation depicted in = Mel Gibson's new film
Apocalypto.=20
So says Gerald Haug of the GeoForschungsZentrum in Germany and
= colleagues, who studied geological records of monsoons over
the past = 16,000 years. They have found a startling
correlation between climate = extremes and the fall of two
great civilisations: the Tang dynasty in = China and the Maya
of South America. "It blew me away," says Haug.
The records show that around the time that these civilizations
went into = decline, they experienced stronger than average
winds in the winter and = weaker summer monsoon rains. These
weak rains would have reduced crop = yields.
Records of monsoons beyond the last 50 years are difficult to
obtain. = Looking for signs of monsoon trends in geological
records going back = thousands of years can help solve this
problem. In China, stalagmites = provide the best available
historical record of summer monsoon rains, = says Haug, as
more rain increases the amount of water dripping down from =
the roofs of caves. But until now, there has been no reliable
estimate = of winter winds.=20
Iron and titanium Haug and his colleagues solved this problem
by studying the sediments = deposited at the bottom of Lake
Hugauang Maar in southeastern China. The = sediments are made
up primarily of material deposited there by winter = monsoon
winds because the catchment area is small, meaning very few =
streams bring in sediments from other sources. As a result,
the = sediments provide an accurate historical record of the
strength of the = winter monsoon winds.
The researchers looked at iron and titanium levels in a
sediment core = that was extracted from the lake floor. The
oxidation level of the iron = told them how much oxygen was
present in the lake waters when the = sediments were
deposited, and therefore how much wind was stirring up = the
lake surface. Titanium in particles is non-reactive and the =
quantities accumulated in the layers of sediment provided
another = measure of wind strength.
When they compared the 16,000 years represented by the mud
core, the = researchers found that years of strong winter
winds corresponded very = closely to strong summer rains and
vice versa. "Our sediment data = provides a mirror image to
summer records in stalagmites," explains = Haug.=20
The researchers believe the only coherent explanation for the
summer and = winter trends and is a shift in the position of a
band of low-pressure = that girdles the Earth, known as the
inter-tropical convergence zone, or = ITCZ.=20
They found that when warm temperatures in the Northern
hemisphere = indicated a northward shift of the ITCZ, summer
monsoon rains were = strong and winter monsoon winds were
weak. "It seems possible that major = shifts in ITCZ catalysed
simultaneous events in civilisations on = opposite sides of
the Pacific Ocean," conclude the researchers in a = paper in
Nature.=20
Catalysing effect Previously, Haug had shown that the
repetitive periods of decline of the = Mayan civilisation in
Latin America corresponded to dry periods on that =
continent.=20
The Maya civilisation and Tang dynasty were contemporary and
there is a = striking similarity between the Chinese and Latin
American climate data. = These include a general shift towards
a drier climate around AD 750 and = three very dry periods
between then and AD 910, the last of which = coincides with
both the Maya and the Tang collapse.
"I am not a historian," cautions Haug, but "there is a
coincidence at = least". He says his work is part of "a
growing piece of evidence that = climate has catalysing effect
on societies".
Analysing historical monsoon records can be extremely useful
in making = future climate predictions. For instance, some
researchers suggest that = strong summer monsoon rains are
preceded by weak winter winds. If true, = this theory could
prove extremely useful in preparing agriculture for a =
difficult year ahead.=20
Journal reference: Nature (vol 445, p 74)
Source: NewScientist http://environment.newscientist.com/arti-
cle/dn10884?DCMP=3DNLC-nletter&ns= ref=3Ddn10884
--=20 Posted by Robert Karl Stonjek
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<HTML><HEAD> <META http-equiv=3DContent-Type
content=3D"text/html; = charset=3Diso-8859-1"> <META
content=3D"MSHTML 6.00.3790.1218" name=3DGENERATOR>
<STYLE></STYLE> </HEAD> <BODY> <DIV id=3DartHeadline> <H1
class=3Dinline><FONT size=3D5>Collapse of civilisations linked
to = monsoon=20 changes</FONT></H1></DIV> <UL class=3D"notlist
highlight" id=3Dartdetails>
<LI>11:13 04 January 2007=20
<LII>NewScientist.com news service=20
<LII><A>Catherine Brahic</B> </LI></UL>
<DIV>
<DIW>The downfall of the one of the greatest Chinese
dynasties may have = been=20 catalysed by severe changes
in climate. The same climate changes may = have=20
simultaneously led to the end of the Maya civilisation
depicted in Mel = Gibson's=20 new film
<I>Apocalypto</I>. </P>
<DIX>So says Gerald Haug of the GeoForschungsZentrum in
Germany and = colleagues,=20 who studied geological
records of monsoons over the past 16,000 years. = They
have=20 found a startling correlation between climate
extremes and the fall of = two great=20 civilisations:
the Tang dynasty in China and the Maya of South
America. =
=93It blew=20
me away," says Haug.</P>
<DIY>The records show that around the time that these
civilizations went = into=20 decline, they experienced
stronger than average winds in the winter and = weaker=20
summer monsoon rains. These weak rains would have reduced
crop = yields.</P>
<DIZ>Records of monsoons beyond the last 50 years are
difficult to obtain. = Looking=20 for signs of monsoon
trends in geological records going back thousands = of
years=20 can help solve this problem. In China,
stalagmites provide the best = available=20 historical
record of summer monsoon rains, says Haug, as more rain =
increases the=20 amount of water dripping down from the
roofs of caves. But until now, = there has=20 been no
reliable estimate of winter winds. </P>
<DIZ1><FONT size=3D4>Iron and titanium</FONT></H5>
<DIZ>Haug and his colleagues solved this problem by studying
the sediments =
deposited at the bottom of Lake Hugauang Maar in southeastern
China. The =
sediments are made up primarily of material deposited there by
winter = monsoon=20 winds because the catchment area is small,
meaning very few streams = bring in=20 sediments from other
sources. As a result, the sediments provide an = accurate=20
historical record of the strength of the winter monsoon
winds.</P>
<DIZ>The researchers looked at iron and titanium levels in a
sediment core = that=20 was extracted from the lake
floor. The oxidation level of the iron told = them how=20
much oxygen was present in the lake waters when the
sediments were = deposited,=20 and therefore how much
wind was stirring up the lake surface. Titanium = in=20
particles is non-reactive and the quantities accumulated
in the layers = of=20 sediment provided another measure
of wind strength.</P>
<DIZ>When they compared the 16,000 years represented by the
mud core, the=20 researchers found that years of strong
winter winds corresponded very = closely to=20 strong
summer rains and vice versa. "Our sediment data provides
a mirror = image=20 to summer records in stalagmites,"
explains Haug. </P>
<DIZ>The researchers believe the only coherent explanation for
the summer = and=20 winter trends and is a shift in the
position of a band of low-pressure = that=20 girdles the
Earth, known as the inter-tropical convergence zone, or =
ITCZ. </P>
<DIZ>They found that when warm temperatures in the Northern
hemisphere = indicated a=20 northward shift of the ITCZ,
summer monsoon rains were strong and winter = monsoon=20
winds were weak. "It seems possible that major shifts in
ITCZ catalysed=20 simultaneous events in civilisations on
opposite sides of the Pacific = Ocean,"=20 conclude the
researchers in a paper in <I>Nature</I>. </P>
<DIZ1><FONT size=3D4>Catalysing effect</FONT></H5>
<DIZ>Previously, Haug had shown that the repetitive periods of
decline of = the=20 Mayan civilisation in Latin America
corresponded to dry periods on that=20 continent. </P>
<DIZ>The Maya civilisation and Tang dynasty were contemporary
and there is = a=20 striking similarity between the
Chinese and Latin American climate data. = These=20
include a general shift towards a drier climate around AD
750 and three = very dry=20 periods between then and AD
910, the last of which coincides with both = the Maya=20
and the Tang collapse.</P>
<DIZ>"I am not a historian," cautions Haug, but "there is a
coincidence at = least".=20 He says his work is part of
"a growing piece of evidence that climate = has=20
catalysing effect on societies".</P>
<DIZ>Analysing historical monsoon records can be extremely
useful in = making future=20 climate predictions. For
instance, some researchers suggest that strong =
summer=20 monsoon rains are preceded by weak winter
winds. If true, this theory = could=20 prove extremely
useful in preparing agriculture for a difficult year =
ahead. </P>
<DIZ>Journal reference: <I>Nature</I> (vol 445, p 74)</P>
<DIZ>Source: NewScientist<BR><A=20 href=3D"http://environment-
.newscientist.com/article/dn10884?DCMP=3DNLC-nl= etter&a-
mp;nsref=3Ddn10884">http://environment.newscientist.com/-
article/dn=
10884?DCMP=3DNLC-nletter&nsref=3Ddn10884</A></P>
<DIZ><BR>-- <BR>Posted by<BR>Robert Karl
Stonjek</P></DIV></BODY></HTML>
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