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
Autor*in: |
Bonacci, Ognjen [verfasserIn] |
---|
Format: |
Artikel |
---|---|
Sprache: |
Englisch |
Erschienen: |
2013 |
---|
Schlagwörter: |
---|
Systematik: |
|
---|
Anmerkung: |
© Springer-Verlag Wien 2013 |
---|
Übergeordnetes Werk: |
Enthalten in: Theoretical and applied climatology - Springer Vienna, 1986, 114(2013), 1-2 vom: 26. Jan., Seite 271-279 |
---|---|
Übergeordnetes Werk: |
volume:114 ; year:2013 ; number:1-2 ; day:26 ; month:01 ; pages:271-279 |
Links: |
---|
DOI / URN: |
10.1007/s00704-012-0830-8 |
---|
Katalog-ID: |
OLC2048449891 |
---|
LEADER | 01000caa a22002652 4500 | ||
---|---|---|---|
001 | OLC2048449891 | ||
003 | DE-627 | ||
005 | 20230502135744.0 | ||
007 | tu | ||
008 | 200820s2013 xx ||||| 00| ||eng c | ||
024 | 7 | |a 10.1007/s00704-012-0830-8 |2 doi | |
035 | |a (DE-627)OLC2048449891 | ||
035 | |a (DE-He213)s00704-012-0830-8-p | ||
040 | |a DE-627 |b ger |c DE-627 |e rakwb | ||
041 | |a eng | ||
082 | 0 | 4 | |a 550 |q VZ |
084 | |a 14 |2 ssgn | ||
084 | |a RA 1000 |q VZ |2 rvk | ||
100 | 1 | |a Bonacci, Ognjen |e verfasserin |4 aut | |
245 | 1 | 0 | |a Differences between true mean daily, monthly and annual air temperatures and air temperatures calculated with three equations: a case study from three Croatian stations |
264 | 1 | |c 2013 | |
336 | |a Text |b txt |2 rdacontent | ||
337 | |a ohne Hilfsmittel zu benutzen |b n |2 rdamedia | ||
338 | |a Band |b nc |2 rdacarrier | ||
500 | |a © Springer-Verlag Wien 2013 | ||
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. | ||
650 | 4 | |a Daily Minimum | |
650 | 4 | |a Annual Difference | |
650 | 4 | |a Crop Simulation Model | |
650 | 4 | |a Time Series Homogeneity | |
650 | 4 | |a Cold Mountain | |
700 | 1 | |a Željković, Ivana |4 aut | |
700 | 1 | |a Trogrlić, Robert Šakić |4 aut | |
700 | 1 | |a Milković, Janja |4 aut | |
773 | 0 | 8 | |i Enthalten in |t Theoretical and applied climatology |d Springer Vienna, 1986 |g 114(2013), 1-2 vom: 26. Jan., Seite 271-279 |w (DE-627)129958808 |w (DE-600)405799-5 |w (DE-576)01552857X |x 0177-798X |7 nnns |
773 | 1 | 8 | |g volume:114 |g year:2013 |g number:1-2 |g day:26 |g month:01 |g pages:271-279 |
856 | 4 | 1 | |u https://doi.org/10.1007/s00704-012-0830-8 |z lizenzpflichtig |3 Volltext |
912 | |a GBV_USEFLAG_A | ||
912 | |a SYSFLAG_A | ||
912 | |a GBV_OLC | ||
912 | |a SSG-OLC-GEO | ||
912 | |a SSG-OPC-GGO | ||
912 | |a GBV_ILN_40 | ||
912 | |a GBV_ILN_70 | ||
912 | |a GBV_ILN_4012 | ||
912 | |a GBV_ILN_4313 | ||
936 | r | v | |a RA 1000 |
951 | |a AR | ||
952 | |d 114 |j 2013 |e 1-2 |b 26 |c 01 |h 271-279 |
author_variant |
o b ob i ž iž r š t rš ršt j m jm |
---|---|
matchkey_str |
article:0177798X:2013----::ifrnebtenreenalmnhynanaareprtrsnareprtrsacltdihheeut |
hierarchy_sort_str |
2013 |
publishDate |
2013 |
allfields |
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 |
spelling |
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 |
allfields_unstemmed |
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 |
allfieldsGer |
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 |
allfieldsSound |
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 |
language |
English |
source |
Enthalten in Theoretical and applied climatology 114(2013), 1-2 vom: 26. Jan., Seite 271-279 volume:114 year:2013 number:1-2 day:26 month:01 pages:271-279 |
sourceStr |
Enthalten in Theoretical and applied climatology 114(2013), 1-2 vom: 26. Jan., Seite 271-279 volume:114 year:2013 number:1-2 day:26 month:01 pages:271-279 |
format_phy_str_mv |
Article |
institution |
findex.gbv.de |
topic_facet |
Daily Minimum Annual Difference Crop Simulation Model Time Series Homogeneity Cold Mountain |
dewey-raw |
550 |
isfreeaccess_bool |
false |
container_title |
Theoretical and applied climatology |
authorswithroles_txt_mv |
Bonacci, Ognjen @@aut@@ Željković, Ivana @@aut@@ Trogrlić, Robert Šakić @@aut@@ Milković, Janja @@aut@@ |
publishDateDaySort_date |
2013-01-26T00:00:00Z |
hierarchy_top_id |
129958808 |
dewey-sort |
3550 |
id |
OLC2048449891 |
language_de |
englisch |
fullrecord |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">OLC2048449891</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230502135744.0</controlfield><controlfield tag="007">tu</controlfield><controlfield tag="008">200820s2013 xx ||||| 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/s00704-012-0830-8</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)OLC2048449891</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-He213)s00704-012-0830-8-p</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">14</subfield><subfield code="2">ssgn</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">RA 1000</subfield><subfield code="q">VZ</subfield><subfield code="2">rvk</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Bonacci, Ognjen</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Differences between true mean daily, monthly and annual air temperatures and air temperatures calculated with three equations: a case study from three Croatian stations</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2013</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">ohne Hilfsmittel zu benutzen</subfield><subfield code="b">n</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Band</subfield><subfield code="b">nc</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">© Springer-Verlag Wien 2013</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="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.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Daily Minimum</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Annual Difference</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Crop Simulation Model</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Time Series Homogeneity</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Cold Mountain</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Željković, Ivana</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Trogrlić, Robert Šakić</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Milković, Janja</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Theoretical and applied climatology</subfield><subfield code="d">Springer Vienna, 1986</subfield><subfield code="g">114(2013), 1-2 vom: 26. Jan., Seite 271-279</subfield><subfield code="w">(DE-627)129958808</subfield><subfield code="w">(DE-600)405799-5</subfield><subfield code="w">(DE-576)01552857X</subfield><subfield code="x">0177-798X</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:114</subfield><subfield code="g">year:2013</subfield><subfield code="g">number:1-2</subfield><subfield code="g">day:26</subfield><subfield code="g">month:01</subfield><subfield code="g">pages:271-279</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">https://doi.org/10.1007/s00704-012-0830-8</subfield><subfield code="z">lizenzpflichtig</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_OLC</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-GEO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-GGO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_40</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_70</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4012</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4313</subfield></datafield><datafield tag="936" ind1="r" ind2="v"><subfield code="a">RA 1000</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">114</subfield><subfield code="j">2013</subfield><subfield code="e">1-2</subfield><subfield code="b">26</subfield><subfield code="c">01</subfield><subfield code="h">271-279</subfield></datafield></record></collection>
|
author |
Bonacci, Ognjen |
spellingShingle |
Bonacci, Ognjen ddc 550 ssgn 14 rvk RA 1000 misc Daily Minimum misc Annual Difference misc Crop Simulation Model misc Time Series Homogeneity misc Cold Mountain Differences between true mean daily, monthly and annual air temperatures and air temperatures calculated with three equations: a case study from three Croatian stations |
authorStr |
Bonacci, Ognjen |
ppnlink_with_tag_str_mv |
@@773@@(DE-627)129958808 |
format |
Article |
dewey-ones |
550 - Earth sciences |
delete_txt_mv |
keep |
author_role |
aut aut aut aut |
collection |
OLC |
remote_str |
false |
illustrated |
Not Illustrated |
issn |
0177-798X |
topic_title |
550 VZ 14 ssgn RA 1000 VZ rvk Differences between true mean daily, monthly and annual air temperatures and air temperatures calculated with three equations: a case study from three Croatian stations Daily Minimum Annual Difference Crop Simulation Model Time Series Homogeneity Cold Mountain |
topic |
ddc 550 ssgn 14 rvk RA 1000 misc Daily Minimum misc Annual Difference misc Crop Simulation Model misc Time Series Homogeneity misc Cold Mountain |
topic_unstemmed |
ddc 550 ssgn 14 rvk RA 1000 misc Daily Minimum misc Annual Difference misc Crop Simulation Model misc Time Series Homogeneity misc Cold Mountain |
topic_browse |
ddc 550 ssgn 14 rvk RA 1000 misc Daily Minimum misc Annual Difference misc Crop Simulation Model misc Time Series Homogeneity misc Cold Mountain |
format_facet |
Aufsätze Gedruckte Aufsätze |
format_main_str_mv |
Text Zeitschrift/Artikel |
carriertype_str_mv |
nc |
hierarchy_parent_title |
Theoretical and applied climatology |
hierarchy_parent_id |
129958808 |
dewey-tens |
550 - Earth sciences & geology |
hierarchy_top_title |
Theoretical and applied climatology |
isfreeaccess_txt |
false |
familylinks_str_mv |
(DE-627)129958808 (DE-600)405799-5 (DE-576)01552857X |
title |
Differences between true mean daily, monthly and annual air temperatures and air temperatures calculated with three equations: a case study from three Croatian stations |
ctrlnum |
(DE-627)OLC2048449891 (DE-He213)s00704-012-0830-8-p |
title_full |
Differences between true mean daily, monthly and annual air temperatures and air temperatures calculated with three equations: a case study from three Croatian stations |
author_sort |
Bonacci, Ognjen |
journal |
Theoretical and applied climatology |
journalStr |
Theoretical and applied climatology |
lang_code |
eng |
isOA_bool |
false |
dewey-hundreds |
500 - Science |
recordtype |
marc |
publishDateSort |
2013 |
contenttype_str_mv |
txt |
container_start_page |
271 |
author_browse |
Bonacci, Ognjen Željković, Ivana Trogrlić, Robert Šakić Milković, Janja |
container_volume |
114 |
class |
550 VZ 14 ssgn RA 1000 VZ rvk |
format_se |
Aufsätze |
author-letter |
Bonacci, Ognjen |
doi_str_mv |
10.1007/s00704-012-0830-8 |
dewey-full |
550 |
title_sort |
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 |
collection_details |
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 |
container_issue |
1-2 |
title_short |
Differences between true mean daily, monthly and annual air temperatures and air temperatures calculated with three equations: a case study from three Croatian stations |
url |
https://doi.org/10.1007/s00704-012-0830-8 |
remote_bool |
false |
author2 |
Željković, Ivana Trogrlić, Robert Šakić Milković, Janja |
author2Str |
Željković, Ivana Trogrlić, Robert Šakić Milković, Janja |
ppnlink |
129958808 |
mediatype_str_mv |
n |
isOA_txt |
false |
hochschulschrift_bool |
false |
doi_str |
10.1007/s00704-012-0830-8 |
up_date |
2024-07-03T18:46:48.625Z |
_version_ |
1803584702908465152 |
fullrecord_marcxml |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">OLC2048449891</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230502135744.0</controlfield><controlfield tag="007">tu</controlfield><controlfield tag="008">200820s2013 xx ||||| 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/s00704-012-0830-8</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)OLC2048449891</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-He213)s00704-012-0830-8-p</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">14</subfield><subfield code="2">ssgn</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">RA 1000</subfield><subfield code="q">VZ</subfield><subfield code="2">rvk</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Bonacci, Ognjen</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Differences between true mean daily, monthly and annual air temperatures and air temperatures calculated with three equations: a case study from three Croatian stations</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2013</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">ohne Hilfsmittel zu benutzen</subfield><subfield code="b">n</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Band</subfield><subfield code="b">nc</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">© Springer-Verlag Wien 2013</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="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.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Daily Minimum</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Annual Difference</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Crop Simulation Model</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Time Series Homogeneity</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Cold Mountain</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Željković, Ivana</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Trogrlić, Robert Šakić</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Milković, Janja</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Theoretical and applied climatology</subfield><subfield code="d">Springer Vienna, 1986</subfield><subfield code="g">114(2013), 1-2 vom: 26. Jan., Seite 271-279</subfield><subfield code="w">(DE-627)129958808</subfield><subfield code="w">(DE-600)405799-5</subfield><subfield code="w">(DE-576)01552857X</subfield><subfield code="x">0177-798X</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:114</subfield><subfield code="g">year:2013</subfield><subfield code="g">number:1-2</subfield><subfield code="g">day:26</subfield><subfield code="g">month:01</subfield><subfield code="g">pages:271-279</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">https://doi.org/10.1007/s00704-012-0830-8</subfield><subfield code="z">lizenzpflichtig</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_OLC</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-GEO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-GGO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_40</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_70</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4012</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4313</subfield></datafield><datafield tag="936" ind1="r" ind2="v"><subfield code="a">RA 1000</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">114</subfield><subfield code="j">2013</subfield><subfield code="e">1-2</subfield><subfield code="b">26</subfield><subfield code="c">01</subfield><subfield code="h">271-279</subfield></datafield></record></collection>
|
score |
7.3995314 |