Estimation of Tigris-Euphrates streamflow from regional paleoenvironmental proxy data
Abstract A six thousand year history of streamflow in Mesopotamia is derived from a synthesis of regional paleoenvironmental proxy data. The proxy data are interpreted with consideration to the climatic signals represented in the records and to the temporal resolution of the records. A consideration...
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| Autor*in: |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
1981 |
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| Umfang: |
13 |
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| Reproduktion: |
Springer Online Journal Archives 1860-2002 |
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| Übergeordnetes Werk: |
in: Climatic change - 1977, 3(1981) vom: März, Seite 251-263 |
| Übergeordnetes Werk: |
volume:3 ; year:1981 ; month:03 ; pages:251-263 ; extent:13 |
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| 520 | |a Abstract A six thousand year history of streamflow in Mesopotamia is derived from a synthesis of regional paleoenvironmental proxy data. The proxy data are interpreted with consideration to the climatic signals represented in the records and to the temporal resolution of the records. A consideration of modern synoptic climatology suggests the spatial patterns of streamflow-generating precipitation in relation to atmospheric circulation. These patterns provide a framework for the interpretation of streamflow from the regional proxies. Given the nature of the data at hand, only a low frequency signal is reconstructed. Assessment of the role of small scale climatic fluctuations as a forcing function of population dynamics must await the availability of finer resolution environmental data. | ||
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(DE-627)NLEJ193613603 DE-627 ger DE-627 rakwb eng Estimation of Tigris-Euphrates streamflow from regional paleoenvironmental proxy data 1981 13 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Abstract A six thousand year history of streamflow in Mesopotamia is derived from a synthesis of regional paleoenvironmental proxy data. The proxy data are interpreted with consideration to the climatic signals represented in the records and to the temporal resolution of the records. A consideration of modern synoptic climatology suggests the spatial patterns of streamflow-generating precipitation in relation to atmospheric circulation. These patterns provide a framework for the interpretation of streamflow from the regional proxies. Given the nature of the data at hand, only a low frequency signal is reconstructed. Assessment of the role of small scale climatic fluctuations as a forcing function of population dynamics must await the availability of finer resolution environmental data. Springer Online Journal Archives 1860-2002 Kay, Paul A. oth Johnson, Douglas L. oth in Climatic change 1977 3(1981) vom: März, Seite 251-263 (DE-627)NLEJ188987371 (DE-600)1477652-2 1573-1480 nnns volume:3 year:1981 month:03 pages:251-263 extent:13 http://dx.doi.org/10.1007/BF00136671 GBV_USEFLAG_U ZDB-1-SOJ GBV_NL_ARTICLE AR 3 1981 3 251-263 13 |
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(DE-627)NLEJ193613603 DE-627 ger DE-627 rakwb eng Estimation of Tigris-Euphrates streamflow from regional paleoenvironmental proxy data 1981 13 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Abstract A six thousand year history of streamflow in Mesopotamia is derived from a synthesis of regional paleoenvironmental proxy data. The proxy data are interpreted with consideration to the climatic signals represented in the records and to the temporal resolution of the records. A consideration of modern synoptic climatology suggests the spatial patterns of streamflow-generating precipitation in relation to atmospheric circulation. These patterns provide a framework for the interpretation of streamflow from the regional proxies. Given the nature of the data at hand, only a low frequency signal is reconstructed. Assessment of the role of small scale climatic fluctuations as a forcing function of population dynamics must await the availability of finer resolution environmental data. Springer Online Journal Archives 1860-2002 Kay, Paul A. oth Johnson, Douglas L. oth in Climatic change 1977 3(1981) vom: März, Seite 251-263 (DE-627)NLEJ188987371 (DE-600)1477652-2 1573-1480 nnns volume:3 year:1981 month:03 pages:251-263 extent:13 http://dx.doi.org/10.1007/BF00136671 GBV_USEFLAG_U ZDB-1-SOJ GBV_NL_ARTICLE AR 3 1981 3 251-263 13 |
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(DE-627)NLEJ193613603 DE-627 ger DE-627 rakwb eng Estimation of Tigris-Euphrates streamflow from regional paleoenvironmental proxy data 1981 13 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Abstract A six thousand year history of streamflow in Mesopotamia is derived from a synthesis of regional paleoenvironmental proxy data. The proxy data are interpreted with consideration to the climatic signals represented in the records and to the temporal resolution of the records. A consideration of modern synoptic climatology suggests the spatial patterns of streamflow-generating precipitation in relation to atmospheric circulation. These patterns provide a framework for the interpretation of streamflow from the regional proxies. Given the nature of the data at hand, only a low frequency signal is reconstructed. Assessment of the role of small scale climatic fluctuations as a forcing function of population dynamics must await the availability of finer resolution environmental data. Springer Online Journal Archives 1860-2002 Kay, Paul A. oth Johnson, Douglas L. oth in Climatic change 1977 3(1981) vom: März, Seite 251-263 (DE-627)NLEJ188987371 (DE-600)1477652-2 1573-1480 nnns volume:3 year:1981 month:03 pages:251-263 extent:13 http://dx.doi.org/10.1007/BF00136671 GBV_USEFLAG_U ZDB-1-SOJ GBV_NL_ARTICLE AR 3 1981 3 251-263 13 |
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(DE-627)NLEJ193613603 DE-627 ger DE-627 rakwb eng Estimation of Tigris-Euphrates streamflow from regional paleoenvironmental proxy data 1981 13 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Abstract A six thousand year history of streamflow in Mesopotamia is derived from a synthesis of regional paleoenvironmental proxy data. The proxy data are interpreted with consideration to the climatic signals represented in the records and to the temporal resolution of the records. A consideration of modern synoptic climatology suggests the spatial patterns of streamflow-generating precipitation in relation to atmospheric circulation. These patterns provide a framework for the interpretation of streamflow from the regional proxies. Given the nature of the data at hand, only a low frequency signal is reconstructed. Assessment of the role of small scale climatic fluctuations as a forcing function of population dynamics must await the availability of finer resolution environmental data. Springer Online Journal Archives 1860-2002 Kay, Paul A. oth Johnson, Douglas L. oth in Climatic change 1977 3(1981) vom: März, Seite 251-263 (DE-627)NLEJ188987371 (DE-600)1477652-2 1573-1480 nnns volume:3 year:1981 month:03 pages:251-263 extent:13 http://dx.doi.org/10.1007/BF00136671 GBV_USEFLAG_U ZDB-1-SOJ GBV_NL_ARTICLE AR 3 1981 3 251-263 13 |
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(DE-627)NLEJ193613603 DE-627 ger DE-627 rakwb eng Estimation of Tigris-Euphrates streamflow from regional paleoenvironmental proxy data 1981 13 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Abstract A six thousand year history of streamflow in Mesopotamia is derived from a synthesis of regional paleoenvironmental proxy data. The proxy data are interpreted with consideration to the climatic signals represented in the records and to the temporal resolution of the records. A consideration of modern synoptic climatology suggests the spatial patterns of streamflow-generating precipitation in relation to atmospheric circulation. These patterns provide a framework for the interpretation of streamflow from the regional proxies. Given the nature of the data at hand, only a low frequency signal is reconstructed. Assessment of the role of small scale climatic fluctuations as a forcing function of population dynamics must await the availability of finer resolution environmental data. Springer Online Journal Archives 1860-2002 Kay, Paul A. oth Johnson, Douglas L. oth in Climatic change 1977 3(1981) vom: März, Seite 251-263 (DE-627)NLEJ188987371 (DE-600)1477652-2 1573-1480 nnns volume:3 year:1981 month:03 pages:251-263 extent:13 http://dx.doi.org/10.1007/BF00136671 GBV_USEFLAG_U ZDB-1-SOJ GBV_NL_ARTICLE AR 3 1981 3 251-263 13 |
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Estimation of Tigris-Euphrates streamflow from regional paleoenvironmental proxy data |
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Abstract A six thousand year history of streamflow in Mesopotamia is derived from a synthesis of regional paleoenvironmental proxy data. The proxy data are interpreted with consideration to the climatic signals represented in the records and to the temporal resolution of the records. A consideration of modern synoptic climatology suggests the spatial patterns of streamflow-generating precipitation in relation to atmospheric circulation. These patterns provide a framework for the interpretation of streamflow from the regional proxies. Given the nature of the data at hand, only a low frequency signal is reconstructed. Assessment of the role of small scale climatic fluctuations as a forcing function of population dynamics must await the availability of finer resolution environmental data. |
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Abstract A six thousand year history of streamflow in Mesopotamia is derived from a synthesis of regional paleoenvironmental proxy data. The proxy data are interpreted with consideration to the climatic signals represented in the records and to the temporal resolution of the records. A consideration of modern synoptic climatology suggests the spatial patterns of streamflow-generating precipitation in relation to atmospheric circulation. These patterns provide a framework for the interpretation of streamflow from the regional proxies. Given the nature of the data at hand, only a low frequency signal is reconstructed. Assessment of the role of small scale climatic fluctuations as a forcing function of population dynamics must await the availability of finer resolution environmental data. |
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Abstract A six thousand year history of streamflow in Mesopotamia is derived from a synthesis of regional paleoenvironmental proxy data. The proxy data are interpreted with consideration to the climatic signals represented in the records and to the temporal resolution of the records. A consideration of modern synoptic climatology suggests the spatial patterns of streamflow-generating precipitation in relation to atmospheric circulation. These patterns provide a framework for the interpretation of streamflow from the regional proxies. Given the nature of the data at hand, only a low frequency signal is reconstructed. Assessment of the role of small scale climatic fluctuations as a forcing function of population dynamics must await the availability of finer resolution environmental data. |
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