New Zealand climate: The temperature record, historical data and some agricultural implications
Abstract Evidence is presented that suggests that annual and seasonal temperatures are in phase throughout the New Zealand region for climatic variation. Annual and seasonal temperature curves dating back to 1853 based on the longest instrumental records show a warming of over 1 °C between the early...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Salinger, M. J. [verfasserIn] |
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| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
1979 |
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| Schlagwörter: |
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| Systematik: |
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| Anmerkung: |
© D. Reidel Publishing Company 1979 |
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| Übergeordnetes Werk: |
Enthalten in: Climatic change - Kluwer Academic Publishers, 1977, 2(1979), 2 vom: Juni, Seite 109-126 |
|---|---|
| Übergeordnetes Werk: |
volume:2 ; year:1979 ; number:2 ; month:06 ; pages:109-126 |
| Links: |
|---|
| DOI / URN: |
10.1007/BF00133218 |
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| Katalog-ID: |
OLC2062574878 |
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| 520 | |a Abstract Evidence is presented that suggests that annual and seasonal temperatures are in phase throughout the New Zealand region for climatic variation. Annual and seasonal temperature curves dating back to 1853 based on the longest instrumental records show a warming of over 1 °C between the early 1860's and the present day, with a 0.5 °C discontinuity since the mid 1940's. Although the warming is regional, the magnitude and timing of the fluctuations vary because of the country's high relief, and wide latitude range. These factors give differing exposure to the atmosphere and oceanic circulations, the resultant interaction of which allows the country to be divided into six temperature response areas which are homogeneous for fluctuations. The information of the last fifty years in these areas is compared. The story from the longer record is supported by phenomena documented from historical sources such as glacial variations, iceberg sightings, and severe snowstorm occurrences. The length and intensity of the growing season is examined in two climatically different areas of New Zealand to ascertain the agricultural significance of the described climate record. | ||
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10.1007/BF00133218 doi (DE-627)OLC2062574878 (DE-He213)BF00133218-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn RA 1000 VZ rvk Salinger, M. J. verfasserin aut New Zealand climate: The temperature record, historical data and some agricultural implications 1979 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © D. Reidel Publishing Company 1979 Abstract Evidence is presented that suggests that annual and seasonal temperatures are in phase throughout the New Zealand region for climatic variation. Annual and seasonal temperature curves dating back to 1853 based on the longest instrumental records show a warming of over 1 °C between the early 1860's and the present day, with a 0.5 °C discontinuity since the mid 1940's. Although the warming is regional, the magnitude and timing of the fluctuations vary because of the country's high relief, and wide latitude range. These factors give differing exposure to the atmosphere and oceanic circulations, the resultant interaction of which allows the country to be divided into six temperature response areas which are homogeneous for fluctuations. The information of the last fifty years in these areas is compared. The story from the longer record is supported by phenomena documented from historical sources such as glacial variations, iceberg sightings, and severe snowstorm occurrences. The length and intensity of the growing season is examined in two climatically different areas of New Zealand to ascertain the agricultural significance of the described climate record. Temperature Response Temperature Curve Oceanic Circulation Temperature Record Seasonal Temperature Enthalten in Climatic change Kluwer Academic Publishers, 1977 2(1979), 2 vom: Juni, Seite 109-126 (DE-627)130479020 (DE-600)751086-X (DE-576)016068610 0165-0009 nnns volume:2 year:1979 number:2 month:06 pages:109-126 https://doi.org/10.1007/BF00133218 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-UMW SSG-OLC-GEO SSG-OLC-IBL SSG-OPC-GGO GBV_ILN_22 GBV_ILN_40 GBV_ILN_70 GBV_ILN_130 GBV_ILN_601 GBV_ILN_2003 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2015 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4103 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4305 GBV_ILN_4311 GBV_ILN_4319 GBV_ILN_4325 RA 1000 AR 2 1979 2 06 109-126 |
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10.1007/BF00133218 doi (DE-627)OLC2062574878 (DE-He213)BF00133218-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn RA 1000 VZ rvk Salinger, M. J. verfasserin aut New Zealand climate: The temperature record, historical data and some agricultural implications 1979 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © D. Reidel Publishing Company 1979 Abstract Evidence is presented that suggests that annual and seasonal temperatures are in phase throughout the New Zealand region for climatic variation. Annual and seasonal temperature curves dating back to 1853 based on the longest instrumental records show a warming of over 1 °C between the early 1860's and the present day, with a 0.5 °C discontinuity since the mid 1940's. Although the warming is regional, the magnitude and timing of the fluctuations vary because of the country's high relief, and wide latitude range. These factors give differing exposure to the atmosphere and oceanic circulations, the resultant interaction of which allows the country to be divided into six temperature response areas which are homogeneous for fluctuations. The information of the last fifty years in these areas is compared. The story from the longer record is supported by phenomena documented from historical sources such as glacial variations, iceberg sightings, and severe snowstorm occurrences. The length and intensity of the growing season is examined in two climatically different areas of New Zealand to ascertain the agricultural significance of the described climate record. Temperature Response Temperature Curve Oceanic Circulation Temperature Record Seasonal Temperature Enthalten in Climatic change Kluwer Academic Publishers, 1977 2(1979), 2 vom: Juni, Seite 109-126 (DE-627)130479020 (DE-600)751086-X (DE-576)016068610 0165-0009 nnns volume:2 year:1979 number:2 month:06 pages:109-126 https://doi.org/10.1007/BF00133218 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-UMW SSG-OLC-GEO SSG-OLC-IBL SSG-OPC-GGO GBV_ILN_22 GBV_ILN_40 GBV_ILN_70 GBV_ILN_130 GBV_ILN_601 GBV_ILN_2003 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2015 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4103 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4305 GBV_ILN_4311 GBV_ILN_4319 GBV_ILN_4325 RA 1000 AR 2 1979 2 06 109-126 |
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10.1007/BF00133218 doi (DE-627)OLC2062574878 (DE-He213)BF00133218-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn RA 1000 VZ rvk Salinger, M. J. verfasserin aut New Zealand climate: The temperature record, historical data and some agricultural implications 1979 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © D. Reidel Publishing Company 1979 Abstract Evidence is presented that suggests that annual and seasonal temperatures are in phase throughout the New Zealand region for climatic variation. Annual and seasonal temperature curves dating back to 1853 based on the longest instrumental records show a warming of over 1 °C between the early 1860's and the present day, with a 0.5 °C discontinuity since the mid 1940's. Although the warming is regional, the magnitude and timing of the fluctuations vary because of the country's high relief, and wide latitude range. These factors give differing exposure to the atmosphere and oceanic circulations, the resultant interaction of which allows the country to be divided into six temperature response areas which are homogeneous for fluctuations. The information of the last fifty years in these areas is compared. The story from the longer record is supported by phenomena documented from historical sources such as glacial variations, iceberg sightings, and severe snowstorm occurrences. The length and intensity of the growing season is examined in two climatically different areas of New Zealand to ascertain the agricultural significance of the described climate record. Temperature Response Temperature Curve Oceanic Circulation Temperature Record Seasonal Temperature Enthalten in Climatic change Kluwer Academic Publishers, 1977 2(1979), 2 vom: Juni, Seite 109-126 (DE-627)130479020 (DE-600)751086-X (DE-576)016068610 0165-0009 nnns volume:2 year:1979 number:2 month:06 pages:109-126 https://doi.org/10.1007/BF00133218 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-UMW SSG-OLC-GEO SSG-OLC-IBL SSG-OPC-GGO GBV_ILN_22 GBV_ILN_40 GBV_ILN_70 GBV_ILN_130 GBV_ILN_601 GBV_ILN_2003 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2015 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4103 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4305 GBV_ILN_4311 GBV_ILN_4319 GBV_ILN_4325 RA 1000 AR 2 1979 2 06 109-126 |
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10.1007/BF00133218 doi (DE-627)OLC2062574878 (DE-He213)BF00133218-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn RA 1000 VZ rvk Salinger, M. J. verfasserin aut New Zealand climate: The temperature record, historical data and some agricultural implications 1979 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © D. Reidel Publishing Company 1979 Abstract Evidence is presented that suggests that annual and seasonal temperatures are in phase throughout the New Zealand region for climatic variation. Annual and seasonal temperature curves dating back to 1853 based on the longest instrumental records show a warming of over 1 °C between the early 1860's and the present day, with a 0.5 °C discontinuity since the mid 1940's. Although the warming is regional, the magnitude and timing of the fluctuations vary because of the country's high relief, and wide latitude range. These factors give differing exposure to the atmosphere and oceanic circulations, the resultant interaction of which allows the country to be divided into six temperature response areas which are homogeneous for fluctuations. The information of the last fifty years in these areas is compared. The story from the longer record is supported by phenomena documented from historical sources such as glacial variations, iceberg sightings, and severe snowstorm occurrences. The length and intensity of the growing season is examined in two climatically different areas of New Zealand to ascertain the agricultural significance of the described climate record. Temperature Response Temperature Curve Oceanic Circulation Temperature Record Seasonal Temperature Enthalten in Climatic change Kluwer Academic Publishers, 1977 2(1979), 2 vom: Juni, Seite 109-126 (DE-627)130479020 (DE-600)751086-X (DE-576)016068610 0165-0009 nnns volume:2 year:1979 number:2 month:06 pages:109-126 https://doi.org/10.1007/BF00133218 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-UMW SSG-OLC-GEO SSG-OLC-IBL SSG-OPC-GGO GBV_ILN_22 GBV_ILN_40 GBV_ILN_70 GBV_ILN_130 GBV_ILN_601 GBV_ILN_2003 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2015 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4103 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4305 GBV_ILN_4311 GBV_ILN_4319 GBV_ILN_4325 RA 1000 AR 2 1979 2 06 109-126 |
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10.1007/BF00133218 doi (DE-627)OLC2062574878 (DE-He213)BF00133218-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn RA 1000 VZ rvk Salinger, M. J. verfasserin aut New Zealand climate: The temperature record, historical data and some agricultural implications 1979 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © D. Reidel Publishing Company 1979 Abstract Evidence is presented that suggests that annual and seasonal temperatures are in phase throughout the New Zealand region for climatic variation. Annual and seasonal temperature curves dating back to 1853 based on the longest instrumental records show a warming of over 1 °C between the early 1860's and the present day, with a 0.5 °C discontinuity since the mid 1940's. Although the warming is regional, the magnitude and timing of the fluctuations vary because of the country's high relief, and wide latitude range. These factors give differing exposure to the atmosphere and oceanic circulations, the resultant interaction of which allows the country to be divided into six temperature response areas which are homogeneous for fluctuations. The information of the last fifty years in these areas is compared. The story from the longer record is supported by phenomena documented from historical sources such as glacial variations, iceberg sightings, and severe snowstorm occurrences. The length and intensity of the growing season is examined in two climatically different areas of New Zealand to ascertain the agricultural significance of the described climate record. Temperature Response Temperature Curve Oceanic Circulation Temperature Record Seasonal Temperature Enthalten in Climatic change Kluwer Academic Publishers, 1977 2(1979), 2 vom: Juni, Seite 109-126 (DE-627)130479020 (DE-600)751086-X (DE-576)016068610 0165-0009 nnns volume:2 year:1979 number:2 month:06 pages:109-126 https://doi.org/10.1007/BF00133218 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-UMW SSG-OLC-GEO SSG-OLC-IBL SSG-OPC-GGO GBV_ILN_22 GBV_ILN_40 GBV_ILN_70 GBV_ILN_130 GBV_ILN_601 GBV_ILN_2003 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2015 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4103 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4305 GBV_ILN_4311 GBV_ILN_4319 GBV_ILN_4325 RA 1000 AR 2 1979 2 06 109-126 |
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550 VZ 14 ssgn RA 1000 VZ rvk New Zealand climate: The temperature record, historical data and some agricultural implications Temperature Response Temperature Curve Oceanic Circulation Temperature Record Seasonal Temperature |
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New Zealand climate: The temperature record, historical data and some agricultural implications |
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New Zealand climate: The temperature record, historical data and some agricultural implications |
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Salinger, M. J. |
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Climatic change |
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Salinger, M. J. |
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10.1007/BF00133218 |
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550 |
| title_sort |
new zealand climate: the temperature record, historical data and some agricultural implications |
| title_auth |
New Zealand climate: The temperature record, historical data and some agricultural implications |
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Abstract Evidence is presented that suggests that annual and seasonal temperatures are in phase throughout the New Zealand region for climatic variation. Annual and seasonal temperature curves dating back to 1853 based on the longest instrumental records show a warming of over 1 °C between the early 1860's and the present day, with a 0.5 °C discontinuity since the mid 1940's. Although the warming is regional, the magnitude and timing of the fluctuations vary because of the country's high relief, and wide latitude range. These factors give differing exposure to the atmosphere and oceanic circulations, the resultant interaction of which allows the country to be divided into six temperature response areas which are homogeneous for fluctuations. The information of the last fifty years in these areas is compared. The story from the longer record is supported by phenomena documented from historical sources such as glacial variations, iceberg sightings, and severe snowstorm occurrences. The length and intensity of the growing season is examined in two climatically different areas of New Zealand to ascertain the agricultural significance of the described climate record. © D. Reidel Publishing Company 1979 |
| abstractGer |
Abstract Evidence is presented that suggests that annual and seasonal temperatures are in phase throughout the New Zealand region for climatic variation. Annual and seasonal temperature curves dating back to 1853 based on the longest instrumental records show a warming of over 1 °C between the early 1860's and the present day, with a 0.5 °C discontinuity since the mid 1940's. Although the warming is regional, the magnitude and timing of the fluctuations vary because of the country's high relief, and wide latitude range. These factors give differing exposure to the atmosphere and oceanic circulations, the resultant interaction of which allows the country to be divided into six temperature response areas which are homogeneous for fluctuations. The information of the last fifty years in these areas is compared. The story from the longer record is supported by phenomena documented from historical sources such as glacial variations, iceberg sightings, and severe snowstorm occurrences. The length and intensity of the growing season is examined in two climatically different areas of New Zealand to ascertain the agricultural significance of the described climate record. © D. Reidel Publishing Company 1979 |
| abstract_unstemmed |
Abstract Evidence is presented that suggests that annual and seasonal temperatures are in phase throughout the New Zealand region for climatic variation. Annual and seasonal temperature curves dating back to 1853 based on the longest instrumental records show a warming of over 1 °C between the early 1860's and the present day, with a 0.5 °C discontinuity since the mid 1940's. Although the warming is regional, the magnitude and timing of the fluctuations vary because of the country's high relief, and wide latitude range. These factors give differing exposure to the atmosphere and oceanic circulations, the resultant interaction of which allows the country to be divided into six temperature response areas which are homogeneous for fluctuations. The information of the last fifty years in these areas is compared. The story from the longer record is supported by phenomena documented from historical sources such as glacial variations, iceberg sightings, and severe snowstorm occurrences. The length and intensity of the growing season is examined in two climatically different areas of New Zealand to ascertain the agricultural significance of the described climate record. © D. Reidel Publishing Company 1979 |
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New Zealand climate: The temperature record, historical data and some agricultural implications |
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