The influence of climatic factors on tree-ring width of Siberian larch in the upper basin of Irtysh river

European beech (Fagus sylvatica L.) adapts to local growing conditions to enhance its performance. In response to variations in climatic conditions, beech trees adjust leaf phenology, cambial phenology, and wood formation patterns, which result in different tree-ring widths (TRWs) and wood anatomy. Chronologies of tree ring width and vessel features [i.e., mean vessel area (MVA), vessel density (VD), and relative conductive area (RCTA)] were produced for the 1960–2016 period for three sites that differ in climatic regimes and spring leaf phenology (two early- and one late-flushing populations). These data were used to investigate long-term relationships between climatic conditions and anatomical features of four quarters of tree-rings at annual and intra-annual scales. In addition, we investigated how TRW and vessel features adjust in response to extreme weather events (i.e., summer drought). We found significant differences in TRW, VD, and RCTA among the selected sites. Precipitation and maximum temperature before and during the growing season were the most important climatic factors affecting TRW and vessel characteristics. We confirmed differences in climate-growth relationships between the selected sites, late flushing beech population at Idrija showing the least pronounced response to climate. MVA was the only vessel trait that showed no relationship with TRW or other vessel features. The relationship between MVA and climatic factors evaluated at intra-annual scale indicated that vessel area in the first quarter of tree-ring were mainly influenced by climatic conditions in the previous growing season, while vessel area in the second to fourth quarters of tree ring width was mainly influenced by maximum temperature and precipitation in the current growing season. When comparing wet and dry years, beech from all sites showed a similar response, with reduced TRW and changes in intra-annual variation in vessel area. Our findings suggest that changes in temperature and precipitation regimes as predicted by most climate change scenarios will affect tree-ring increments and wood structure in beech, yet the response between sites or populations may differ.

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Dendrochronological analysis and growth patterns of Polylepis reticulata (Rosaceae) in the Ecuadorian Andes

IAWA Journal ◽

10.1163/22941932-40190240 ◽

2019 ◽

Vol 40 (2) ◽

pp. 331-S5 ◽

Cited By ~ 3

Author(s):

C. Alvites ◽

G. Battipaglia ◽

G. Santopuoli ◽

H. Hampel ◽

R.F. Vázquez ◽

...

Keyword(s):

Tree Ring ◽

Tree Rings ◽

Stand Structure ◽

Climatic Factors ◽

Southern Oscillation ◽

Ring Width ◽

Vapour Pressure Deficit ◽

Growth Patterns ◽

Tree Ring Width ◽

Sources Of Information

ABSTRACTRelict tree species in the Andean mountains are important sources of information about climate variability and climate change. This study deals with dendroclimatology and growth patterns in Polylepis reticulata Hieron., growing at high elevation (mean of 4000 m a.s.l.) in three sites of the Ecuadorian Andes. The aims of the research were: (i) characterizing tree-ring boundaries; (ii) describing tree-ring patterns of the study sites; (iii) investigating the relationships between climate and radial tree growth; and (iv) determining the spatial correlation between seasonal climatic factors and tree-ring width of P. reticulata. Tree rings were characterized by semi-ring porosity and slight differences in fibre wall thickness between latewood and subsequent earlywood. In all sampling sites, tree rings in heartwood were more clearly visible than in sapwood. Tree-ring width was more related to temperature than to precipitation, with growth being also affected by site conditions and stand structure, as well as other local factors. No significant relationships were found between tree-ring chronologies of P. reticulata and El Niño-Southern Oscillation (ENSO) and Vapour Pressure Deficit indices. The study highlights that there is not a clear driving climate factor for radial growth of P. reticulata. Additional research is needed to study growth dynamics of this species and the impacts of local environmental variables.

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Climatic factors controlling reproduction and growth of Norway spruce in southern Norway

Canadian Journal of Forest Research ◽

10.1139/x01-192 ◽

2002 ◽

Vol 32 (2) ◽

pp. 217-225 ◽

Cited By ~ 89

Author(s):

Vidar Selås ◽

Gianluca Piovesan ◽

Jonathan M Adams ◽

Mauro Bernabei

Keyword(s):

Norway Spruce ◽

Seed Production ◽

Tree Ring ◽

Climatic Factors ◽

Statistical Significance ◽

Ring Width ◽

Tree Ring Width ◽

Late Spring Frost ◽

Southern Norway ◽

June July

Time series of seed production and tree-ring width of Norway spruce (Picea abies (L.) Karst.) in southern Norway were analysed for their relationship to various climatic factors occurring during "key" stages, which a priori might be expected to show a strong climate response. The following factors combined in a multiple linear regression model were found to predict seed production (based on withheld data points) with considerable accuracy, at high levels of statistical significance: JuneJuly mean temperature and August lowest temperature in the previous year, late spring frost and JuneJuly precipitation of the last 2 years, and JanuaryFebruary lowest temperature in the current year. Tree ring width was negatively correlated with the seed production index of the current year and the lowest July temperature in the previous year and positively correlated with June-July precipitation in the current year. It is suggested that habitat constraints for seedling establishment should also be considered in a more general life-history cost theory to explain masting behaviour in forest trees.

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Relation of tree-ring width and earlywood vessel size of alien Quercus rubra L. with climatic factors in Latvia

Silva Fennica ◽

10.14214/sf.1391 ◽

2015 ◽

Vol 49 (4) ◽

Cited By ~ 6

Author(s):

Roberts Matisons ◽

Jānis Jansons ◽

Juris Katrevičs ◽

Āris Jansons

Keyword(s):

Tree Ring ◽

Quercus Rubra ◽

Climatic Factors ◽

Ring Width ◽

Tree Ring Width ◽

Vessel Size ◽

Earlywood Vessel

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Effects of extreme drought and wet events for tree mortality: Insights from tree‐ring width and carbon isotope ratio in a Siberian larch forest

Ecohydrology ◽

10.1002/eco.2143 ◽

2019 ◽

Vol 12 (8) ◽

Cited By ~ 4

Author(s):

Shunsuke Tei ◽

Atsuko Sugimoto ◽

Hitoshi Yonenobu ◽

Ayumi Kotani ◽

Trofim C. Maximov

Keyword(s):

Carbon Isotope ◽

Tree Ring ◽

Isotope Ratio ◽

Tree Mortality ◽

Ring Width ◽

Siberian Larch ◽

Carbon Isotope Ratio ◽

Larch Forest ◽

Extreme Drought ◽

Tree Ring Width

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A Method for Reconstructing the Past Soil Temperature Based on Tree-Ring Widths

Forest Science ◽

10.1093/forsci/fxaa001 ◽

2020 ◽

Vol 66 (4) ◽

pp. 393-402

Author(s):

Shuai Yuan ◽

Yonghong Zheng ◽

Yongdong Qi ◽

Fanxi Kong ◽

Dan Wang ◽

...

Keyword(s):

Soil Temperature ◽

Tree Ring ◽

Climatic Factors ◽

Ring Width ◽

Reconstruction Method ◽

Dabie Mountains ◽

Tree Ring Width ◽

Soil Temperatures ◽

High Elevations

Abstract Soil temperature can affect tree growth and is one of the most important types of basic data for forest cultivation and management. To obtain a long-term time series of soil temperatures, we explored the utility of dendroclimatology in a subtropical area of China. In this study, the relations between tree-ring-width chronologies and climate factors were explored by correlation analysis. The results indicated that the limiting climatic factors for the radial growth of Huangshan pine were elevation-specific. Further investigation found that chronology at high elevations was significantly correlated with soil temperature. Then, we described a reconstruction of the soil temperatures of the Dabie Mountains area using the tree-ring width chronology from 1869 to 2015 and showed that the reconstruction explained 42.9 percent of the instrumental soil temperature variation in the common years. We found that the 1970s and 2000s were the coldest and warmest decades since 1884, respectively. The results of the reconstruction method for describing past soil temperatures can provide a reference for other subtropical forests. Furthermore, the results of our research also have a certain significance for guiding policymaking related to forest cultivation and management.

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On the ‘Divergence Problem’ in the Alatau Mountains, Central Asia: A Study of the Responses of Schrenk Spruce Tree-Ring Width to Climate under the Recent Warming and Wetting Trend

Atmosphere ◽

10.3390/atmos10080473 ◽

2019 ◽

Vol 10 (8) ◽

pp. 473 ◽

Cited By ~ 3

Author(s):

Zhang ◽

Jiang ◽

Bagila ◽

Ainur ◽

...

Keyword(s):

Central Asia ◽

Tree Ring ◽

Tree Growth ◽

Tree Species ◽

Climatic Factors ◽

Ring Width ◽

Tree Ring Width ◽

Recent Warming ◽

Divergence Problem ◽

The Stability

The divergence problem, which manifests as an unstable response relationship between tree-ring growth and climatic factors under the background of global warming, poses a challenge to both the traditional theory of dendroclimatology and the reliability of climatic reconstructions based on tree-ring data. Although Schrenk spruce, as the dominant tree species in the Tianshan Mountains, is frequently applied in the dendrochronological studies, the understanding of the divergence problem of this tree species is still limited. This study conducted correlation analysis between climatic factors and tree-ring width chronologies from 51 living and healthy specimens of Schrenk spruce at sites of high and low elevation in the Alatau Mountains to determine the stability of the response. The results revealed that the tree-ring width of the spruce specimens was correlated positively with precipitation and correlated negatively with temperature. Although the variations of the two tree-ring chronologies were similar, the radial growth of the spruce at the low elevation was found more sensitive to climatic factors. Furthermore, the sensitivity of tree growth to climate demonstrated an obvious increase after an abrupt change of climate under the background of the recent warming and wetting trend. Increased drought stress, calculated based on climatic data, was regarded as the main reason for this phenomenon. The results supply the gap of the stability of climatic response of tree growth in Central Asia to some extent.

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Effect of climatic factors on tree-ring width of Populus hybrids in Latvia

Silva Fennica ◽

10.14214/sf.1442 ◽

2016 ◽

Vol 50 (1) ◽

Cited By ~ 2

Author(s):

Silva Šēnhofa ◽

Mārtiņš Zeps ◽

Roberts Matisons ◽

Jānis Smilga ◽

Dagnija Lazdiņa ◽

...

Keyword(s):

Tree Ring ◽

Climatic Factors ◽

Ring Width ◽

Tree Ring Width

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Early summer temperatures since 1670 A.D. for Central Kamchatka reconstructed based on a Siberian larch tree-ring width chronology

Canadian Journal of Forest Research ◽

10.1139/x26-230 ◽

1996 ◽

Vol 26 (11) ◽

pp. 2048-2052 ◽

Cited By ~ 33

Author(s):

Moses Gostev ◽

Gregory Wiles ◽

Rosanne D'Arrigo ◽

Gordon Jacoby ◽

Peter Khomentovsky

Keyword(s):

Tree Ring ◽

Ring Width ◽

Siberian Larch ◽

Kamchatka Peninsula ◽

Early Summer ◽

Model Verification ◽

Tree Ring Width ◽

Tree Ring Data ◽

Summer Temperatures ◽

Larch Tree

A tree-ring width chronology of larch (Larixkurilensis Mayr) has been developed from along the Bystraya River near Esso in the interior valley of the Kamchatka Peninsula, Russia. The chronology, which covers from 1670 to 1992, explains 38% of the variance in May–June temperatures for the Esso meteorological station. This ring-width series is used to develop the first dendroclimatic reconstruction for Kamchatka. We caution that the Esso station record, the closest to the tree-ring site, is only 42 years in length, making model verification difficult. Periods of above-average temperatures are inferred for ca. 1750, 1800, and over the last few decades; colder than average conditions are inferred for 1710–1720, 1760–1770s, and 1860–1880s. The ring-width chronology cross-dates with other larch tree-ring data for Kamchatka and, during certain intervals, with a larch ring-width record from eastern Siberia. Comparison of the two records suggests that the insertion of a missing ring for the year 1816 in the eastern Siberian series is not justified. A birch (Betulaermanii Cham.) chronology from a coastal site near Petropavlovsk-Kamchatskiy correlates with July–August temperatures. Both the larch and more widespread birch species show promise for further dendroclimatic studies in Kamchatka.

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Changes in the Tree-Ring Width-Derived Cumulative Normalized Difference Vegetation Index over Northeast China during 1825 to 2013 CE

Forests ◽

10.3390/f12020241 ◽

2021 ◽

Vol 12 (2) ◽

pp. 241

Author(s):

Ruoshi Liu ◽

Yi Song ◽

Yu Liu ◽

Xuxiang Li ◽

Huiming Song ◽

...

Keyword(s):

Tree Ring ◽

Vegetation Index ◽

Normalized Difference Vegetation Index ◽

Climatic Factors ◽

Eastern China ◽

Ring Width ◽

Terrestrial Ecosystems ◽

Vegetation Coverage ◽

Drought Severity ◽

Tree Ring Width

Vegetation coverage is very important in terrestrial ecosystems and climate systems. However, the observational record of the normalized difference vegetation index (NDVI), which started in the 1980s when satellites became widely used, is too short to investigate the history of variation in vegetation coverage beyond the modern observation period. Here, we present a 189 y vegetation coverage series based on a total of 349 Mongolian pine (Pinus sylvestris var. mongolica Litv) cores from seven locations from the central–western Da Hinggan Mountains (CW–DHM), northeastern China. We found a significant relationship between tree-ring width and the regional cumulative normalized difference vegetation index (CNDVI). The correlation between the ring-width chronology and the regional June–July CNDVI (CNDVIJJ) was significant, with r = 0.68 (n = 32, p < 0.001) and an explained variance of 45.8% (44.0% after the adjustment for the loss of the degree of freedom). On this basis, we designed a transfer function to reconstruct the CNDVIJJ for the CW–DHM region from 1825 to 2013 CE (Common Era). During the last 189 years, there were 28 years with high CNDVIJJ values, and another 28 years with low values. We also observed CNDVIJJ fluctuations at the inter-annual and decadal time scales, including eight low value periods and nine high value periods. Based on our analysis, the variation in CNDVI is associated with climatic factors, such as temperature, precipitation and the Palmer Drought Severity Index (PDSI), which combines both temperature and precipitation. From 1950 to 2002 CE, the CNDVI showed a noticeable decreasing trend in the CW–DHM region, whereas after 2003 CE, the CNDVI exhibited an apparent increase, which has also been observed in southern Central Siberia, eastern Mongolia and northeastern and eastern China, indicating that the CNDVI change in the CW–DHM is related to climate change in the local region and in some parts of Asia.

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