Precipitation measurements by manual and automatic rain gauges and their influence on homogeneity of long-term precipitation series
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F86652079%3A_____%2F21%3A00542188" target="_blank" >RIV/86652079:_____/21:00542188 - isvavai.cz</a>
Nalezeny alternativní kódy
RIV/00020699:_____/20:N0000151 RIV/00216224:14310/21:00120881
Výsledek na webu
<a href="https://rmets.onlinelibrary.wiley.com/doi/epdf/10.1002/joc.6862" target="_blank" >https://rmets.onlinelibrary.wiley.com/doi/epdf/10.1002/joc.6862</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1002/joc.6862" target="_blank" >10.1002/joc.6862</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Precipitation measurements by manual and automatic rain gauges and their influence on homogeneity of long-term precipitation series
Popis výsledku v původním jazyce
The introduction of automatic instruments for precipitation measurements may have resulted in some differences in results from those taken by previous manual instruments. In the station network of the Czech Hydrometeorological Institute (CHMI) this replacement process began in the 1990s, when precipitation measurements taken by the METRA 886 rain gauge gave way to automatic tipping-bucket rain gauges, the MR3H and later the MR3H-FC. Continuous simultaneous measurement by both types of rain gauge at the Brno-Zabovresky and Ostrava-Poruba stations in the 2000-2019 period enable differences in recorded daily precipitation totals to be compared. Only those days upon which at least one of the two types of rain gauge recorded precipitation are analysed herein. Although the highest proportion of differences in daily precipitation totals lies between0.1 and 0.1 mm, there is a distinct tendency towards higher totals in positive deviations as measured by the manual METRA 886, that is, tipping-bucket rain gauges generally record lower precipitation totals then the 'standard' manual rain gauge (the MR3H-FC undervalues totals to a greater extent than the MR3H). The design and construction of tipping-bucket rain gauges are reflected in overvaluation of precipitation days with smaller totals and undervaluation of days with high totals when compared with the METRA 886. Series combining measurements by METRA 886 and by tipping-bucket rain gauges (as held in the CHMI database) and series measured by the METRA 886 alone were created, homogenized and analysed in terms of long-term fluctuations and annual variations. Homogenisation of precipitation series based on combined measurements leads to generally undervalued totals compared with those measured only by the METRA 886. Results are discussed with respect to other similar articles, sources of errors in both types of precipitation measurement, and with regard to the homogenisation of precipitation series.
Název v anglickém jazyce
Precipitation measurements by manual and automatic rain gauges and their influence on homogeneity of long-term precipitation series
Popis výsledku anglicky
The introduction of automatic instruments for precipitation measurements may have resulted in some differences in results from those taken by previous manual instruments. In the station network of the Czech Hydrometeorological Institute (CHMI) this replacement process began in the 1990s, when precipitation measurements taken by the METRA 886 rain gauge gave way to automatic tipping-bucket rain gauges, the MR3H and later the MR3H-FC. Continuous simultaneous measurement by both types of rain gauge at the Brno-Zabovresky and Ostrava-Poruba stations in the 2000-2019 period enable differences in recorded daily precipitation totals to be compared. Only those days upon which at least one of the two types of rain gauge recorded precipitation are analysed herein. Although the highest proportion of differences in daily precipitation totals lies between0.1 and 0.1 mm, there is a distinct tendency towards higher totals in positive deviations as measured by the manual METRA 886, that is, tipping-bucket rain gauges generally record lower precipitation totals then the 'standard' manual rain gauge (the MR3H-FC undervalues totals to a greater extent than the MR3H). The design and construction of tipping-bucket rain gauges are reflected in overvaluation of precipitation days with smaller totals and undervaluation of days with high totals when compared with the METRA 886. Series combining measurements by METRA 886 and by tipping-bucket rain gauges (as held in the CHMI database) and series measured by the METRA 886 alone were created, homogenized and analysed in terms of long-term fluctuations and annual variations. Homogenisation of precipitation series based on combined measurements leads to generally undervalued totals compared with those measured only by the METRA 886. Results are discussed with respect to other similar articles, sources of errors in both types of precipitation measurement, and with regard to the homogenisation of precipitation series.
Klasifikace
Druh
J<sub>imp</sub> - Článek v periodiku v databázi Web of Science
CEP obor
—
OECD FORD obor
10509 - Meteorology and atmospheric sciences
Návaznosti výsledku
Projekt
<a href="/cs/project/EF16_019%2F0000797" target="_blank" >EF16_019/0000797: SustES - Adaptační strategie pro udržitelnost ekosystémových služeb a potravinové bezpečnosti v nepříznivých přírodních podmínkách</a><br>
Návaznosti
P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)
Ostatní
Rok uplatnění
2021
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
International Journal of Climatology
ISSN
0899-8418
e-ISSN
1097-0088
Svazek periodika
41
Číslo periodika v rámci svazku
JAN
Stát vydavatele periodika
GB - Spojené království Velké Británie a Severního Irska
Počet stran výsledku
15
Strana od-do
"E2537"-"E2552"
Kód UT WoS článku
000586313900001
EID výsledku v databázi Scopus
2-s2.0-85092493912