Andrew Lorrey
Biographic Data
| ID | 5597189 |
|---|---|
| NAME | Andrew Lorrey |
| GIVEN NAMES | Andrew |
| FAMILY NAME | Lorrey |
| SIGNATURE | LORREY A |
| AFFILIATIONS | National Institute of Water and Atmospheric Research (NIWA), Auckland, New Zealand |
| VERIFIED | No |
| TOTAL WORKS | 9 |
| TOTAL CITATIONS | 19 |
| AUTHOR COUNT | 9 |
| EDITOR COUNT | 0 |
| FIRST PUBLICATION YEAR | 2005 |
| LATEST PUBLICATION YEAR | 2019 |
| H-INDEX | 2 |
Identifying and Quantifying Tree-Ring Chronology Variance Artefacts Related to Co-Occurring Changes in Growth Rate
Expectations that a warming world will be associated with more hydro-climatological extremes has motivated research exploring if an associated signal is evident in paleoclimate archives. Tree-ring chronologies are central to this work because of their high temporal resolution, but they are also potentially compromised by variance artefacts associated with the evolving composition of the chronology and with data processing. Here we present two emp…
Continental-scale temperature variability during the past two millennia
High-resolution modelling of mid-Holocene New Zealand climate at 6000 yr BP
Palaeoclimate-proxy data provide an invaluable source of evidence for past climatic conditions, which can be compared with data from climate model simulations. This study illustrates how high-resolution regional climate model simulations can be used to estimate the difference in the climate of New Zealand between 6000 years before present (yr BP) and the pre-industrial era (c. ad 1750). Four pairs (pre-industrial and 6000 yr BP) of atmosphere-onl…
Late Little Ice Age climate variability in New Zealand documented by the Reverend Davis "Dirty Weather" diaries
Regional climate regime classification and synoptic circulation reconstructions for New Zealand covering the last 2000 years, the mid-Holocene, and the Last Glacial Coldest Period at ∼21Ka
Speleothem stable isotope records interpreted within a multi-proxy framework and implications for New Zealand palaeoclimate reconstruction
Towards a Radiocarbon Calibration for Oxygen Isotope Stage 3 Using New Zealand Kauri ( Agathis Australis )
It is well known that radiocarbon years do not directly equate to calendar time. As a result, considerable effort has been devoted to generating a decadally resolved calibration curve for the Holocene and latter part of the last termination. A calibration curve that can be unambiguously attributed to changes in atmospheric 14 C content has not, however, been generated beyond 26 kyr cal BP, despite the urgent need to rigorously test climatic, envi…
Extension of the New Zealand kauri (Agathis australis) chronology to 1724 BC
Long tree-ring chronologies have been constructed in the Northern Hemisphere for dendroclimatology and palaeoenvironmental studies, radiocarbon calibration and archaeological dating. Numerous tree-ring chronologies have also been built in the Southern Hemisphere, primarily for dendroclimatology, but multimillennial chronologies are rare. Development of long chronologies from the Southern Hemisphere is therefore important to provide a long-term pe…
Seasonal Growth Characteristics of Kauri
Considerable research has occurred in recent years to build Agathis australis (D. Don) Lindley (kauri) tree-ring chronologies for paleoclimate applications and to identify statistical relationships between kauri tree rings and climate. This paper reports on a multi-year study of the seasonal growth of kauri, designed to assist in the interpretation of identified statistical relationships, and to determine if kauri's seasonal growth characteristic…
Extension of the New Zealand kauri (Agathis australis) chronology to 1724 BC
Long tree-ring chronologies have been constructed in the Northern Hemisphere for dendroclimatology and palaeoenvironmental studies, radiocarbon calibration and archaeological dating. Numerous tree-ring chronologies have also been built in the Southern Hemisphere, primarily for dendroclimatology, but multimillennial chronologies are rare. Development of long chronologies from the Southern Hemisphere is therefore important to provide a long-term pe…
Towards a Radiocarbon Calibration for Oxygen Isotope Stage 3 Using New Zealand Kauri ( Agathis Australis )
It is well known that radiocarbon years do not directly equate to calendar time. As a result, considerable effort has been devoted to generating a decadally resolved calibration curve for the Holocene and latter part of the last termination. A calibration curve that can be unambiguously attributed to changes in atmospheric 14 C content has not, however, been generated beyond 26 kyr cal BP, despite the urgent need to rigorously test climatic, envi…
Seasonal Growth Characteristics of Kauri
Considerable research has occurred in recent years to build Agathis australis (D. Don) Lindley (kauri) tree-ring chronologies for paleoclimate applications and to identify statistical relationships between kauri tree rings and climate. This paper reports on a multi-year study of the seasonal growth of kauri, designed to assist in the interpretation of identified statistical relationships, and to determine if kauri's seasonal growth characteristic…
Extension of the New Zealand kauri (Agathis australis) chronology to 1724 BC
Long tree-ring chronologies have been constructed in the Northern Hemisphere for dendroclimatology and palaeoenvironmental studies, radiocarbon calibration and archaeological dating. Numerous tree-ring chronologies have also been built in the Southern Hemisphere, primarily for dendroclimatology, but multimillennial chronologies are rare. Development of long chronologies from the Southern Hemisphere is therefore important to provide a long-term pe…
Towards a Radiocarbon Calibration for Oxygen Isotope Stage 3 Using New Zealand Kauri ( Agathis Australis )
It is well known that radiocarbon years do not directly equate to calendar time. As a result, considerable effort has been devoted to generating a decadally resolved calibration curve for the Holocene and latter part of the last termination. A calibration curve that can be unambiguously attributed to changes in atmospheric 14 C content has not, however, been generated beyond 26 kyr cal BP, despite the urgent need to rigorously test climatic, envi…
Speleothem stable isotope records interpreted within a multi-proxy framework and implications for New Zealand palaeoclimate reconstruction
Late Little Ice Age climate variability in New Zealand documented by the Reverend Davis "Dirty Weather" diaries
Regional climate regime classification and synoptic circulation reconstructions for New Zealand covering the last 2000 years, the mid-Holocene, and the Last Glacial Coldest Period at ∼21Ka
Continental-scale temperature variability during the past two millennia
High-resolution modelling of mid-Holocene New Zealand climate at 6000 yr BP
Palaeoclimate-proxy data provide an invaluable source of evidence for past climatic conditions, which can be compared with data from climate model simulations. This study illustrates how high-resolution regional climate model simulations can be used to estimate the difference in the climate of New Zealand between 6000 years before present (yr BP) and the pre-industrial era (c. ad 1750). Four pairs (pre-industrial and 6000 yr BP) of atmosphere-onl…
Identifying and Quantifying Tree-Ring Chronology Variance Artefacts Related to Co-Occurring Changes in Growth Rate
Expectations that a warming world will be associated with more hydro-climatological extremes has motivated research exploring if an associated signal is evident in paleoclimate archives. Tree-ring chronologies are central to this work because of their high temporal resolution, but they are also potentially compromised by variance artefacts associated with the evolving composition of the chronology and with data processing. Here we present two emp…
Geography (9 works) · Geology and Paleoclimatology Research (9 works) · Climatology (6 works) · Geology (6 works) · Archaeology (5 works) · Pacific and Southeast Asian Studies (5 works) · Physical geography (5 works) · Tree-ring climate responses (5 works) · Climate change (4 works) · Holocene (4 works)