树轮密度对气候的响应及重建研究进展

doi:10.18306/dlkxjz.2021.02.014

Abstract

Abstract:

Tree-ring density is one of the important proxies for climate reconstruction. In the past few decades, international and Chinese scholars have carried out a large number of studies on the relationship between tree-ring density and climate, and many climate series were reconstructed for different regions. In this study, we collected publications about the responses to climate change and climate reconstruction based on tree ring density, and reviewed some progresses in these areas. Although the relationship between tree-ring density and the climate may be affected by tree species, terrain (altitude, slope direction, and so on), and other factors, the maximum latewood density is a well-known proxy of summer or early fall temperature variation in cold and moist areas, while earlywood density can be used to reconstruct precipitation variation in arid areas. Therefore, most of the scholars reconstructed the temperature of the summer or the late fall, and only few precipitation and sea level pressure series were reconstructed based on tree-ring density. In addition, the variance that the reconstruction can explain varies from region to region, and from tree species to species. To date, the reconstruction series spanned 2018 years in Europe, which is the longest in the world, and 449 years in Southwest China, which is the longest series in China. There still exist controversies around the divergence in tree-ring density response to temperature and the cooling effect of volcanic eruptions, because of the unstable relationship between tree-ring density and temperature. Future research should pay more attention to the relationship between tree-ring density and other climate variables such as precipitation and light, and the influence of nonclimatic factors such as altitude, tree species, and experimental methods.

Key words: tree-ring density, climate change, temperature reconstruction, volcanic eruption

DENG Guofu, LI Mingqi. Advances of study on the relationship between tree-ring density and climate and climate reconstruction[J].PROGRESS IN GEOGRAPHY, 2021, 40(2): 343-356.

Figures/Tables 4

Tab.1

International studies on responses of tree-ring density to climate change"

研究区	树种	拉丁名	指标	海拔/m	气候变量	相关系数/时段	文献来源
Pyrenees	欧洲赤松山赤松欧洲冷杉	Pinus sylvestris Pinus uncinata Abies alba	MXD	2010	T(5—9月)	0.80/1952—2002年	[27]
Mount Norikura	富士山冷杉	Abies veitchii	MXD	1600	T(7、9月)	0.30/1979—2005年	[28]
Mount Norikura	富士山冷杉	Abies veitchii	MXD	1900	T(7—9月)	0.35/1979—2005年	[28]
Mount Norikura	大白叶冷杉	Abies mariesii	MXD	1900	T(7—9月)	0.34/1979—2005年	[28]
Mount Norikura	大白叶冷杉	Abies mariesii	MXD	2400	T(7—9月)	0.44/1979—2005年	[28]
Rhaetian Alps, Italy	瑞士五针松	Pinus cembra	MXD	2075~2350	T(5—9月)	0.60/1901—2015年	[29]
Eastern Carpathians	欧洲赤松	Pinus sylvestris	MXD	750~1200	T_max(7月30日—9月24日)	0.63/1961—2013年	[30]
Tatras	欧洲云杉	Picea abies	MXD	1480	T(4—9月)	0.62/1901—2004年	[31]
Dolina Mengusovska	欧洲落叶松	Larix decidua	MXD	1450	T(5—6月)	0.68/1951—2012年	[32]
Village Vernar	欧洲落叶松	Larix decidua	MXD	850	P(7月)	0.43/1951—2012年	[32]
Altai	西伯利亚落叶松	Larix sibirica	MXD	2380	T(6—7月)	0.57/1963—2000年	[33]
Yakutia	卡氏落叶松	Larix cajanderi	MXD	22	T(6—7月)	0.55/1950—2000年	[33]
Alps	欧洲落叶松	Larix decidua	MXD	>1500	T(6—9月)	0.73/1911—2003年	[34]
Franklin Mountains	白云杉	Picea glauca	MXD	653	T(5—8月)	0.45/1944—1977年	[35]
Hornby Cabin	白云杉	Picea glauca	MXD	143	T(5—8月)	0.58/1944—1977年	[35]
Cri Lake	白云杉	Picea glauca	MXD	108	T(5—9月)	0.50/1944—1977年	[35]
Coppermine	白云杉	Picea glauca	MXD	200	T(5—8月)	0.48/1944—1977年	[35]
North-eastern Finland	欧洲赤松	Pinus sylvestris	MXD	200	T(4—9月)	0.68/1876—2013年	[36]
Laanila	欧洲赤松	Pinus sylvestris	MXD	220	T(6—8月)	0.61/1958—2002年	[37]
Suntar Khayata	卡氏落叶松	Larix cajanderi	MXD	900	T_min(6—8月)	0.67/1929—2000年	[38]
Iberian Peninsula	西班牙刺柏	Juniperus thurifera	MID	530~1375	P(4—6月)	-0.67/1951—2000年	[47]
Southern Urals	欧洲赤松	Pinus sylvestris	MID	740	P(5月)	-0.58/1950—2002年	[48]
Khangai	西伯利亚落叶松	Larix sibirica	MID	1920	P(6月)	-0.57/1950—2002年	[48]
Sierra de Gúdar	欧洲黑松	Pinus nigra	MID	1090	P(5月)	-0.65/1950—2002年	[48]

Tab.1

Tab.2

Fig.1

Fig.2

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Advances of study on the relationship between tree-ring density and climate and climate reconstruction

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样点	树种	海拔/m	指标	响应变量	相关系数/时段	文献来源
吉普克	雪岭云杉	2555	MXD	T(8月)	0.35/1959—2004年	[39]
阿乌里亚乔克山	雪岭云杉	2690	MXD	T(4—8月)	0.42/1961—2005年	[39]
小白代沟	雪岭云杉	2682	MXD	T(6—8月)	0.33/1956—2006年	[39]
长白山	长白落叶松	1848	MXD	T_max(6—8月)	0.38/1958—2008年	[40]
长白山	长白落叶松	1585	MXD	T_max(4—9月)	0.44/1958—2008年	[40]
长白山	长白落叶松	983	MXD	T_min(8月)	-0.26/1958—2008年	[40]
漠河	兴安落叶松	650	MXD	T_max(7月)	0.45/1922—1998年	[41]
漠河	兴安落叶松	650	MID	T_min(3月)	-0.323/1922—1998年	[41]
漠河	樟子松	650	MXD	T_max(8月)	0.49/1922—1998年	[41]
漠河	樟子松	650	MID	P(4月)	0.343/1922—1998年	[41]
崆峒山	油松	1950	MID	P(6—8月)	-0.4/1951—2006年	[42]
崆峒山	油松	1950	EWD	P(6—8月)	-0.36/1951—2006年	[42]
崆峒山	油松	1950	MXD	T(6—8月)	-0.26/1951—2006年	[42]
崆峒山	油松	1950	LWD	T(6—9月)	-0.28/1951—2006年	[42]
艾肯达坂	天山云杉	2455	MXD	T(7—8月)	0.30/1968—2005年	[43]
巩乃斯林场北	天山云杉	1982	EWD	P(6—7月)	-0.50/1968—2005年	[43]
艾肯达坂	雪岭云杉	2450	MXD	T_max(5—8月)	0.304/1958—2008年	[44]
小五台山	青杨(雌)	1600	MXD	T_max(8月)	0.348/1982—2011年	[45]
小五台山	青杨(雄)	1600	MXD	T_max(4月)	-0.429/1982—2011年	[45]
祁连山中段	青海云杉	3140~3390	EWD	P(5月)	-0.623/1956—2009年	[49]

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