Cheryl Wood
Biographic Data
| ID | 6450893 |
|---|---|
| NAME | Cheryl Wood |
| GIVEN NAMES | Cheryl |
| FAMILY NAME | Wood |
| SIGNATURE | WOOD C |
| AFFILIATIONS | University of St Andrews |
| VERIFIED | No |
| TOTAL WORKS | 5 |
| TOTAL CITATIONS | 20 |
| AUTHOR COUNT | 5 |
| EDITOR COUNT | 0 |
| FIRST PUBLICATION YEAR | 2008 |
| LATEST PUBLICATION YEAR | 2019 |
| H-INDEX | 3 |
Improved dendroclimatic calibration using blue intensity in the southern Yukon
In north-western North America, the so-called divergence problem (DP) is expressed in tree ring width (RW) as an unstable temperature signal in recent decades. Maximum latewood density (MXD), from the same region, shows minimal evidence of DP. While MXD is a superior proxy for summer temperatures, there are very few long MXD records from North America. Latewood blue intensity (LWB) measures similar wood properties as MXD, expresses a similar clim…
Dendrochronologically Dated Pine Buildings from Scotland
The SCOT2K project has extended native pine tree-ring chronology coverage for Scotland to enable reconstruction of past climate and for cultural heritage dating benefits. Using living trees from multiple locations in the Highlands and sub-fossil material from lochs, a network of five regional chronologies has been produced. The project has developed the application of Blue Intensity (BI), a proxy measure for maximum latewood density, which is fas…
Facilitating tree-ring dating of historic conifer timbers using Blue Intensity
Blue Intensity for dendroclimatology
Maximum latewood density (MXD) is a strong proxy of summer temperatures. Despite this, there is a paucity of long MXD chronologies in the Northern Hemisphere, which limits large-scale tree-ring-based reconstructions of past temperature which are dominated by ring-width (RW) data – a weaker temperature proxy at inter-annual time-scales. This paucity likely results from the relative expense of measuring MXD and the lack of laboratories with the fac…
X-ray microtomographic imaging of charcoal
X-ray microtomographic imaging of charcoal
Facilitating tree-ring dating of historic conifer timbers using Blue Intensity
Blue Intensity for dendroclimatology
Maximum latewood density (MXD) is a strong proxy of summer temperatures. Despite this, there is a paucity of long MXD chronologies in the Northern Hemisphere, which limits large-scale tree-ring-based reconstructions of past temperature which are dominated by ring-width (RW) data – a weaker temperature proxy at inter-annual time-scales. This paucity likely results from the relative expense of measuring MXD and the lack of laboratories with the fac…
Improved dendroclimatic calibration using blue intensity in the southern Yukon
In north-western North America, the so-called divergence problem (DP) is expressed in tree ring width (RW) as an unstable temperature signal in recent decades. Maximum latewood density (MXD), from the same region, shows minimal evidence of DP. While MXD is a superior proxy for summer temperatures, there are very few long MXD records from North America. Latewood blue intensity (LWB) measures similar wood properties as MXD, expresses a similar clim…
Dendrochronologically Dated Pine Buildings from Scotland
The SCOT2K project has extended native pine tree-ring chronology coverage for Scotland to enable reconstruction of past climate and for cultural heritage dating benefits. Using living trees from multiple locations in the Highlands and sub-fossil material from lochs, a network of five regional chronologies has been produced. The project has developed the application of Blue Intensity (BI), a proxy measure for maximum latewood density, which is fas…
X-ray microtomographic imaging of charcoal
Blue Intensity for dendroclimatology
Maximum latewood density (MXD) is a strong proxy of summer temperatures. Despite this, there is a paucity of long MXD chronologies in the Northern Hemisphere, which limits large-scale tree-ring-based reconstructions of past temperature which are dominated by ring-width (RW) data – a weaker temperature proxy at inter-annual time-scales. This paucity likely results from the relative expense of measuring MXD and the lack of laboratories with the fac…
Facilitating tree-ring dating of historic conifer timbers using Blue Intensity
Dendrochronologically Dated Pine Buildings from Scotland
The SCOT2K project has extended native pine tree-ring chronology coverage for Scotland to enable reconstruction of past climate and for cultural heritage dating benefits. Using living trees from multiple locations in the Highlands and sub-fossil material from lochs, a network of five regional chronologies has been produced. The project has developed the application of Blue Intensity (BI), a proxy measure for maximum latewood density, which is fas…
Improved dendroclimatic calibration using blue intensity in the southern Yukon
In north-western North America, the so-called divergence problem (DP) is expressed in tree ring width (RW) as an unstable temperature signal in recent decades. Maximum latewood density (MXD), from the same region, shows minimal evidence of DP. While MXD is a superior proxy for summer temperatures, there are very few long MXD records from North America. Latewood blue intensity (LWB) measures similar wood properties as MXD, expresses a similar clim…
Geography (5 works) · Dendrochronology (4 works) · Geology (4 works) · Physical geography (4 works) · Plant Water Relations and Carbon Dynamics (4 works) · Tree-ring climate responses (4 works) · Archaeology (3 works) · Dendroclimatology (3 works) · Environmental Science (3 works) · Atmospheric sciences (2 works)