Reconstructed Northern Hemisphere annual temperature since 1671 based on high-latitude tree-ring data from North America

1989 ◽  
Vol 14 (1) ◽  
pp. 39-59 ◽  
Author(s):  
Gordon C. Jacoby ◽  
Rosanne D'Arrigo
Keyword(s):  
North America ◽  
Northern Hemisphere ◽  
Tree Ring ◽  
High Latitude ◽  
Tree Ring Data

scholarly journals SHCal20 Southern Hemisphere Calibration, 0–55,000 Years cal BP

Radiocarbon ◽  
2020 ◽  
Vol 62 (4) ◽  
pp. 759-778 ◽  
Author(s):  
Alan G Hogg ◽  
Timothy J Heaton ◽  
Quan Hua ◽  
Jonathan G Palmer ◽  
Chris SM Turney ◽  
...  
Keyword(s):  
Southern Hemisphere ◽  
Northern Hemisphere ◽  
Tree Ring ◽  
Calibration Curve ◽  
Data Sets ◽  
Errors In Variables ◽  
Time Intervals ◽  
Tree Ring Data ◽  
The Mean ◽  
Statistical Approaches

ABSTRACTEarly researchers of radiocarbon levels in Southern Hemisphere tree rings identified a variable North-South hemispheric offset, necessitating construction of a separate radiocarbon calibration curve for the South. We present here SHCal20, a revised calibration curve from 0–55,000 cal BP, based upon SHCal13 and fortified by the addition of 14 new tree-ring data sets in the 2140–0, 3520–3453, 3608–3590 and 13,140–11,375 cal BP time intervals. We detail the statistical approaches used for curve construction and present recommendations for the use of the Northern Hemisphere curve (IntCal20), the Southern Hemisphere curve (SHCal20) and suggest where application of an equal mixture of the curves might be more appropriate. Using our Bayesian spline with errors-in-variables methodology, and based upon a comparison of Southern Hemisphere tree-ring data compared with contemporaneous Northern Hemisphere data, we estimate the mean Southern Hemisphere offset to be 36 ± 27 14C yrs older.

scholarly journals Tree-ring data document 16th century megadrought over North America

Eos ◽  
2000 ◽  
Vol 81 (12) ◽  
pp. 121 ◽  
Author(s):  
David W. Stahle ◽  
Edward R. Cook ◽  
Malcolm K. Cleaveland ◽  
Matthew D. Therrell ◽  
David M. Meko ◽  
...  
Keyword(s):  
North America ◽  
Tree Ring ◽  
16Th Century ◽  
Tree Ring Data

Annual 14C Tree-Ring Data Around 400 AD: Mid- and High-Latitude Records

Radiocarbon ◽  
2019 ◽  
Vol 61 (5) ◽  
pp. 1305-1316 ◽  
Author(s):  
Ronny Friedrich ◽  
Bernd Kromer ◽  
Frank Sirocko ◽  
Jan Esper ◽  
Susanne Lindauer ◽  
...  
Keyword(s):  
Solar Cycle ◽  
Tree Ring ◽  
High Latitude ◽  
Spatial Distance ◽  
Pine Tree ◽  
Solar Cyclicity ◽  
Tree Ring Data ◽  
Oak Tree ◽  
Annual Resolution ◽  
Periodic Changes

ABSTRACTTwo tree-ring series, one from a high-latitude pine tree (located in northern Scandinavia) and one from a mid-latitude oak tree (located in eastern Germany) were analyzed for radiocarbon (14C) at annual resolution. The new records cover the calendar date ranges 290–460 AD and 382–486 AD, respectively, overlapping by 79 yr. The series show similar trends as IntCal13. However, some significant deviations around 400 AD are present with lower Δ14C (higher 14C ages). An average offset between the two new series and IntCal13 of about 20 years in conventional 14C age is observed. A latitudinal 14C offset between the tree sites in central and northern Europe, as would be expected due to the relatively large spatial distance, is not recorded, however. Periodic changes in the 14C records are resolved that can be attributed to the “11-year” solar cycle (Schwabe cycle) with cycle length from 9 to 11 years. The magnitude of changes in Δ14C due to the solar cycle is between 1.5 and 3‰. Since solar cyclicity is only partially synchronous between the two new series, reasons for asynchronicity are explored.

Comparison between Blue Intensity (BI) and Maximum Latewood Density (MXD) tree-ring chronologies from the North American Boreal forests

2020 ◽  
Author(s):  
Laia Andreu-Hayles ◽  
Rosanne D'Arrigo ◽  
Rose Oelkers ◽  
Kevin Anchukaitis ◽  
Greg Wiles ◽  
...  
Keyword(s):  
High Resolution ◽  
North America ◽  
Tree Ring ◽  
Boreal Forests ◽  
Ring Width ◽  
Maximum Latewood Density ◽  
Latewood Density ◽  
Tree Ring Data ◽  
Summer Temperatures ◽  
Blue Intensity

<p>Tree ring-width (TRW) and Maximum Latewood Density (MXD) series have been largely used to develop high-resolution temperature reconstructions for the Northern Hemisphere. The divergence phenomenon, a weakening of the positive relationship between TRW and summer temperatures, has been observed particularly in northwestern North America chronologies. In contrast, MXD datasets have shown a more stable relationship with summer temperatures, but it is costly and labor-intensive to produce. Recently, methodological advances in image analyses have led to development of a less expensive and labor-intensive MXD proxy known as Blue Intensity (BI). Here, we compare 6 newly developed BI tree-ring chronologies of white spruce (<em>Picea glauca</em> [Moench] Voss) from high-latitude boreal forests in North America (Alaska in USA; Yukon and the Northwestern Territory in Canada), with MXD chronologies developed at the same sites. We assessed the quality of BI in relation to MXD based on mean correlation between trees, chronology reliability based on the Expressed Population Signal (EPS), spectral properties, and the strength and spatial extent of the temperature signal. Individual BI chronologies established significant correlations with summer temperatures showing a similar strength and spatial cover than MXD chronologies. Overall, the BI tree-ring data is emerging as a valuable proxy for generating high-resolution temperature spatial reconstructions over northwestern America.</p>

Insect defoliators as major disturbance factors in the high-altitude balsam fir forest of Mount Mégantic, southern Quebec

1998 ◽  
Vol 28 (12) ◽  
pp. 1832-1842 ◽  
Author(s):  
Louise Filion ◽  
Serge Payette ◽  
Ann Delwaide ◽  
Najat Bhiry
Keyword(s):  
North America ◽  
High Altitude ◽  
Tree Ring ◽  
Radial Growth ◽  
Abies Balsamea ◽  
Spruce Budworm ◽  
Balsam Fir ◽  
Cumulative Impact ◽  
Tree Ring Data ◽  
Paper Birch

Tree-ring data from a mature balsam fir forest, located at the top of Mount Mégantic (elevation 1100 m), southern Quebec, suggest that insect defoliators were major disturbance factors in the development of high-altitude balsam fir forests. A comparison between the radial growth trend of balsam fir (Abies balsamea (L.) Mill.), a host species of the spruce budworm (Choristoneura fumiferana Clem.), and paper birch (Betula papyrifera Marsh), a nonhost species, showed that several growth depressions in the balsam fir chronology corrresponded to documented spruce budworm outbreaks in southern Quebec in the 1910s, 1950s, 1970s, and possibly in the 1870s. Tree mortality was extensive during the last infestation because of the relatively old age (>60 years) of many balsam fir and, possibly, to the cumulative impact of defoliation. The tree-ring series from paper birch showed several drops in radial growth after the 1930s, possibly related to the large-scale birch dieback that occurred in eastern North America. Macrofossil data (insect remains) from one sample of the uppermost organic soil layers (F horizon) confirm the presence of the spruce budworm at the study site. The ecological role of insect defoliators is discussed in the context of the high-altitude balsam fir forests in northeastern North America where abiotic disturbances are considered the primary controlling factors in stand dynamics.

Reconstructing Past Climatic Anomalies in the North Pacific and Western North America from Tree-Ring Data

1976 ◽  
Vol 6 (4) ◽  
pp. 563-579 ◽  
Author(s):  
T.J. Blasing ◽  
H.C. Fritts
Keyword(s):  
North America ◽  
19Th Century ◽  
Tree Ring ◽  
North Pacific ◽  
Climatic Conditions ◽  
Climatic Data ◽  
Western North America ◽  
The North ◽  
Tree Ring Data ◽  
The North Pacific

Winter climatic anomalies in the North Pacific sector and western North America are statistically calibrated with tree-ring data in western North America and reconstructed back to AD 1700. The results are verified using climatic data from the last half of the 19th century, which is prior to the calibration period. Climatic conditions reconstructed for 18th and 19th century winters are then summarized and compared with the 20th century record.

Trans-Tasman Sea climate variability since ad 1740 inferred from middle to high latitude tree-ring data

2000 ◽  
Vol 16 (8) ◽  
pp. 603-610 ◽  
Author(s):  
R. D'Arrigo ◽  
E. Cook ◽  
R. Villalba ◽  
B. Buckley ◽  
J. Salinger ◽  
...  
Keyword(s):  
Climate Variability ◽  
Tree Ring ◽  
High Latitude ◽  
Tasman Sea ◽  
Tree Ring Data

scholarly journals Supporting Restoration Decisions through Integration of Tree-Ring and Modeling Data: Reconstructing Flow and Salinity in the San Francisco Estuary over the Past Millennium

Water ◽  
2021 ◽  
Vol 13 (15) ◽  
pp. 2139
Author(s):  
Paul H. Hutton ◽  
David M. Meko ◽  
Sujoy B. Roy
Keyword(s):  
San Francisco ◽  
Tree Ring ◽  
San Francisco Estuary ◽  
Salinity Intrusion ◽  
Estuarine Ecosystem ◽  
Freshwater Flow ◽  
The Past ◽  
Decadal Scale ◽  
Tree Ring Data ◽  
Past Millennium

This work presents updated reconstructions of watershed runoff to San Francisco Estuary from tree-ring data to AD 903, coupled with models relating runoff to freshwater flow to the estuary and salinity intrusion. We characterize pre-development freshwater flow and salinity conditions in the estuary over the past millennium and compare this characterization with contemporary conditions to better understand the magnitude and seasonality of changes over this time. This work shows that the instrumented flow record spans the range of runoff patterns over the past millennium (averaged over 5, 10, 20 and 100 years), and thus serves as a reasonable basis for planning-level evaluations of historical hydrologic conditions in the estuary. Over annual timescales we show that, although median freshwater flow to the estuary has not changed significantly, it has been more variable over the past century compared to pre-development flow conditions. We further show that the contemporary period is generally associated with greater spring salinity intrusion and lesser summer–fall salinity intrusion relative to the pre-development period. Thus, salinity intrusion in summer and fall months was a common occurrence under pre-development conditions and has been moderated in the contemporary period due to the operations of upstream reservoirs, which were designed to hold winter and spring runoff for release in summer and fall. This work also confirms a dramatic decadal-scale hydrologic shift in the watershed from very wet to very dry conditions during the late 19th and early 20th centuries; while not unprecedented, these shifts have been seen only a few times in the past millennium. This shift resulted in an increase in salinity intrusion in the first three decades of the 20th century, as documented through early records. Population growth and extensive watershed modification during this period exacerbated this underlying hydrologic shift. Putting this shift in the context of other anthropogenic drivers is important in understanding the historical response of the estuary and in setting salinity targets for estuarine restoration. By characterizing the long-term behavior of San Francisco Estuary, this work supports decision-making in the State of California related to flow and salinity management for restoration of the estuarine ecosystem.

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