Differences between true mean daily, monthly and annual air temperatures and air temperatures calculated with three equations: a case study from three Croatian stations
Abstract Differences between true mean daily, monthly and annual air temperatures T0 [Eq. (1)] and temperatures calculated with three different equations [(2), (3) and (4)] (commonly used in climatological practice) were investigated at three main meteorological Croatian stations from 1 January 1999...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Bonacci, Ognjen [verfasserIn] |
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| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2013 |
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| Schlagwörter: |
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| Systematik: |
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| Anmerkung: |
© Springer-Verlag Wien 2013 |
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| Übergeordnetes Werk: |
Enthalten in: Theoretical and applied climatology - Springer Vienna, 1986, 114(2013), 1-2 vom: 26. Jan., Seite 271-279 |
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| Übergeordnetes Werk: |
volume:114 ; year:2013 ; number:1-2 ; day:26 ; month:01 ; pages:271-279 |
| Links: |
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| DOI / URN: |
10.1007/s00704-012-0830-8 |
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| Katalog-ID: |
OLC2048449891 |
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| 520 | |a Abstract Differences between true mean daily, monthly and annual air temperatures T0 [Eq. (1)] and temperatures calculated with three different equations [(2), (3) and (4)] (commonly used in climatological practice) were investigated at three main meteorological Croatian stations from 1 January 1999 to 31 December 2011. The stations are situated in the following three climatically distinct areas: (1) Zagreb-Grič (mild continental climate), (2) Zavižan (cold mountain climate), and (3) Dubrovnik (hot Mediterranean climate). T1 [Eq. (2)] and T3 [Eq. (4)] mean temperatures are defined by the algorithms based on the weighted means of temperatures measured at irregularly spaced, yet fixed hours. T2 [Eq. (3)] is the mean temperature defined as the average of daily maximum and minimum temperature. The equation as well as the time of observations used introduces a bias into mean temperatures. The largest differences occur for mean daily temperatures. The calculated daily difference value from all three equations and all analysed stations varies from −3.73 °C to +3.56 °C, from −1.39 °C to +0.79 °C for monthly differences and from −0.76 °C to +0.30 °C for annual differences. | ||
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| 700 | 1 | |a Milković, Janja |4 aut | |
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10.1007/s00704-012-0830-8 doi (DE-627)OLC2048449891 (DE-He213)s00704-012-0830-8-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn RA 1000 VZ rvk Bonacci, Ognjen verfasserin aut Differences between true mean daily, monthly and annual air temperatures and air temperatures calculated with three equations: a case study from three Croatian stations 2013 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag Wien 2013 Abstract Differences between true mean daily, monthly and annual air temperatures T0 [Eq. (1)] and temperatures calculated with three different equations [(2), (3) and (4)] (commonly used in climatological practice) were investigated at three main meteorological Croatian stations from 1 January 1999 to 31 December 2011. The stations are situated in the following three climatically distinct areas: (1) Zagreb-Grič (mild continental climate), (2) Zavižan (cold mountain climate), and (3) Dubrovnik (hot Mediterranean climate). T1 [Eq. (2)] and T3 [Eq. (4)] mean temperatures are defined by the algorithms based on the weighted means of temperatures measured at irregularly spaced, yet fixed hours. T2 [Eq. (3)] is the mean temperature defined as the average of daily maximum and minimum temperature. The equation as well as the time of observations used introduces a bias into mean temperatures. The largest differences occur for mean daily temperatures. The calculated daily difference value from all three equations and all analysed stations varies from −3.73 °C to +3.56 °C, from −1.39 °C to +0.79 °C for monthly differences and from −0.76 °C to +0.30 °C for annual differences. Daily Minimum Annual Difference Crop Simulation Model Time Series Homogeneity Cold Mountain Željković, Ivana aut Trogrlić, Robert Šakić aut Milković, Janja aut Enthalten in Theoretical and applied climatology Springer Vienna, 1986 114(2013), 1-2 vom: 26. Jan., Seite 271-279 (DE-627)129958808 (DE-600)405799-5 (DE-576)01552857X 0177-798X nnns volume:114 year:2013 number:1-2 day:26 month:01 pages:271-279 https://doi.org/10.1007/s00704-012-0830-8 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_40 GBV_ILN_70 GBV_ILN_4012 GBV_ILN_4313 RA 1000 AR 114 2013 1-2 26 01 271-279 |
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10.1007/s00704-012-0830-8 doi (DE-627)OLC2048449891 (DE-He213)s00704-012-0830-8-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn RA 1000 VZ rvk Bonacci, Ognjen verfasserin aut Differences between true mean daily, monthly and annual air temperatures and air temperatures calculated with three equations: a case study from three Croatian stations 2013 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag Wien 2013 Abstract Differences between true mean daily, monthly and annual air temperatures T0 [Eq. (1)] and temperatures calculated with three different equations [(2), (3) and (4)] (commonly used in climatological practice) were investigated at three main meteorological Croatian stations from 1 January 1999 to 31 December 2011. The stations are situated in the following three climatically distinct areas: (1) Zagreb-Grič (mild continental climate), (2) Zavižan (cold mountain climate), and (3) Dubrovnik (hot Mediterranean climate). T1 [Eq. (2)] and T3 [Eq. (4)] mean temperatures are defined by the algorithms based on the weighted means of temperatures measured at irregularly spaced, yet fixed hours. T2 [Eq. (3)] is the mean temperature defined as the average of daily maximum and minimum temperature. The equation as well as the time of observations used introduces a bias into mean temperatures. The largest differences occur for mean daily temperatures. The calculated daily difference value from all three equations and all analysed stations varies from −3.73 °C to +3.56 °C, from −1.39 °C to +0.79 °C for monthly differences and from −0.76 °C to +0.30 °C for annual differences. Daily Minimum Annual Difference Crop Simulation Model Time Series Homogeneity Cold Mountain Željković, Ivana aut Trogrlić, Robert Šakić aut Milković, Janja aut Enthalten in Theoretical and applied climatology Springer Vienna, 1986 114(2013), 1-2 vom: 26. Jan., Seite 271-279 (DE-627)129958808 (DE-600)405799-5 (DE-576)01552857X 0177-798X nnns volume:114 year:2013 number:1-2 day:26 month:01 pages:271-279 https://doi.org/10.1007/s00704-012-0830-8 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_40 GBV_ILN_70 GBV_ILN_4012 GBV_ILN_4313 RA 1000 AR 114 2013 1-2 26 01 271-279 |
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10.1007/s00704-012-0830-8 doi (DE-627)OLC2048449891 (DE-He213)s00704-012-0830-8-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn RA 1000 VZ rvk Bonacci, Ognjen verfasserin aut Differences between true mean daily, monthly and annual air temperatures and air temperatures calculated with three equations: a case study from three Croatian stations 2013 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag Wien 2013 Abstract Differences between true mean daily, monthly and annual air temperatures T0 [Eq. (1)] and temperatures calculated with three different equations [(2), (3) and (4)] (commonly used in climatological practice) were investigated at three main meteorological Croatian stations from 1 January 1999 to 31 December 2011. The stations are situated in the following three climatically distinct areas: (1) Zagreb-Grič (mild continental climate), (2) Zavižan (cold mountain climate), and (3) Dubrovnik (hot Mediterranean climate). T1 [Eq. (2)] and T3 [Eq. (4)] mean temperatures are defined by the algorithms based on the weighted means of temperatures measured at irregularly spaced, yet fixed hours. T2 [Eq. (3)] is the mean temperature defined as the average of daily maximum and minimum temperature. The equation as well as the time of observations used introduces a bias into mean temperatures. The largest differences occur for mean daily temperatures. The calculated daily difference value from all three equations and all analysed stations varies from −3.73 °C to +3.56 °C, from −1.39 °C to +0.79 °C for monthly differences and from −0.76 °C to +0.30 °C for annual differences. Daily Minimum Annual Difference Crop Simulation Model Time Series Homogeneity Cold Mountain Željković, Ivana aut Trogrlić, Robert Šakić aut Milković, Janja aut Enthalten in Theoretical and applied climatology Springer Vienna, 1986 114(2013), 1-2 vom: 26. Jan., Seite 271-279 (DE-627)129958808 (DE-600)405799-5 (DE-576)01552857X 0177-798X nnns volume:114 year:2013 number:1-2 day:26 month:01 pages:271-279 https://doi.org/10.1007/s00704-012-0830-8 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_40 GBV_ILN_70 GBV_ILN_4012 GBV_ILN_4313 RA 1000 AR 114 2013 1-2 26 01 271-279 |
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10.1007/s00704-012-0830-8 doi (DE-627)OLC2048449891 (DE-He213)s00704-012-0830-8-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn RA 1000 VZ rvk Bonacci, Ognjen verfasserin aut Differences between true mean daily, monthly and annual air temperatures and air temperatures calculated with three equations: a case study from three Croatian stations 2013 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag Wien 2013 Abstract Differences between true mean daily, monthly and annual air temperatures T0 [Eq. (1)] and temperatures calculated with three different equations [(2), (3) and (4)] (commonly used in climatological practice) were investigated at three main meteorological Croatian stations from 1 January 1999 to 31 December 2011. The stations are situated in the following three climatically distinct areas: (1) Zagreb-Grič (mild continental climate), (2) Zavižan (cold mountain climate), and (3) Dubrovnik (hot Mediterranean climate). T1 [Eq. (2)] and T3 [Eq. (4)] mean temperatures are defined by the algorithms based on the weighted means of temperatures measured at irregularly spaced, yet fixed hours. T2 [Eq. (3)] is the mean temperature defined as the average of daily maximum and minimum temperature. The equation as well as the time of observations used introduces a bias into mean temperatures. The largest differences occur for mean daily temperatures. The calculated daily difference value from all three equations and all analysed stations varies from −3.73 °C to +3.56 °C, from −1.39 °C to +0.79 °C for monthly differences and from −0.76 °C to +0.30 °C for annual differences. Daily Minimum Annual Difference Crop Simulation Model Time Series Homogeneity Cold Mountain Željković, Ivana aut Trogrlić, Robert Šakić aut Milković, Janja aut Enthalten in Theoretical and applied climatology Springer Vienna, 1986 114(2013), 1-2 vom: 26. Jan., Seite 271-279 (DE-627)129958808 (DE-600)405799-5 (DE-576)01552857X 0177-798X nnns volume:114 year:2013 number:1-2 day:26 month:01 pages:271-279 https://doi.org/10.1007/s00704-012-0830-8 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_40 GBV_ILN_70 GBV_ILN_4012 GBV_ILN_4313 RA 1000 AR 114 2013 1-2 26 01 271-279 |
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Differences between true mean daily, monthly and annual air temperatures and air temperatures calculated with three equations: a case study from three Croatian stations |
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Differences between true mean daily, monthly and annual air temperatures and air temperatures calculated with three equations: a case study from three Croatian stations |
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Bonacci, Ognjen |
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Theoretical and applied climatology |
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2013 |
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Bonacci, Ognjen Željković, Ivana Trogrlić, Robert Šakić Milković, Janja |
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10.1007/s00704-012-0830-8 |
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550 |
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differences between true mean daily, monthly and annual air temperatures and air temperatures calculated with three equations: a case study from three croatian stations |
| title_auth |
Differences between true mean daily, monthly and annual air temperatures and air temperatures calculated with three equations: a case study from three Croatian stations |
| abstract |
Abstract Differences between true mean daily, monthly and annual air temperatures T0 [Eq. (1)] and temperatures calculated with three different equations [(2), (3) and (4)] (commonly used in climatological practice) were investigated at three main meteorological Croatian stations from 1 January 1999 to 31 December 2011. The stations are situated in the following three climatically distinct areas: (1) Zagreb-Grič (mild continental climate), (2) Zavižan (cold mountain climate), and (3) Dubrovnik (hot Mediterranean climate). T1 [Eq. (2)] and T3 [Eq. (4)] mean temperatures are defined by the algorithms based on the weighted means of temperatures measured at irregularly spaced, yet fixed hours. T2 [Eq. (3)] is the mean temperature defined as the average of daily maximum and minimum temperature. The equation as well as the time of observations used introduces a bias into mean temperatures. The largest differences occur for mean daily temperatures. The calculated daily difference value from all three equations and all analysed stations varies from −3.73 °C to +3.56 °C, from −1.39 °C to +0.79 °C for monthly differences and from −0.76 °C to +0.30 °C for annual differences. © Springer-Verlag Wien 2013 |
| abstractGer |
Abstract Differences between true mean daily, monthly and annual air temperatures T0 [Eq. (1)] and temperatures calculated with three different equations [(2), (3) and (4)] (commonly used in climatological practice) were investigated at three main meteorological Croatian stations from 1 January 1999 to 31 December 2011. The stations are situated in the following three climatically distinct areas: (1) Zagreb-Grič (mild continental climate), (2) Zavižan (cold mountain climate), and (3) Dubrovnik (hot Mediterranean climate). T1 [Eq. (2)] and T3 [Eq. (4)] mean temperatures are defined by the algorithms based on the weighted means of temperatures measured at irregularly spaced, yet fixed hours. T2 [Eq. (3)] is the mean temperature defined as the average of daily maximum and minimum temperature. The equation as well as the time of observations used introduces a bias into mean temperatures. The largest differences occur for mean daily temperatures. The calculated daily difference value from all three equations and all analysed stations varies from −3.73 °C to +3.56 °C, from −1.39 °C to +0.79 °C for monthly differences and from −0.76 °C to +0.30 °C for annual differences. © Springer-Verlag Wien 2013 |
| abstract_unstemmed |
Abstract Differences between true mean daily, monthly and annual air temperatures T0 [Eq. (1)] and temperatures calculated with three different equations [(2), (3) and (4)] (commonly used in climatological practice) were investigated at three main meteorological Croatian stations from 1 January 1999 to 31 December 2011. The stations are situated in the following three climatically distinct areas: (1) Zagreb-Grič (mild continental climate), (2) Zavižan (cold mountain climate), and (3) Dubrovnik (hot Mediterranean climate). T1 [Eq. (2)] and T3 [Eq. (4)] mean temperatures are defined by the algorithms based on the weighted means of temperatures measured at irregularly spaced, yet fixed hours. T2 [Eq. (3)] is the mean temperature defined as the average of daily maximum and minimum temperature. The equation as well as the time of observations used introduces a bias into mean temperatures. The largest differences occur for mean daily temperatures. The calculated daily difference value from all three equations and all analysed stations varies from −3.73 °C to +3.56 °C, from −1.39 °C to +0.79 °C for monthly differences and from −0.76 °C to +0.30 °C for annual differences. © Springer-Verlag Wien 2013 |
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Differences between true mean daily, monthly and annual air temperatures and air temperatures calculated with three equations: a case study from three Croatian stations |
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Željković, Ivana Trogrlić, Robert Šakić Milković, Janja |
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