FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2912155001> ?p ?o ?g. }

• W2912155001 endingPage "68" @default.
• W2912155001 startingPage "68" @default.
• W2912155001 abstract "This article presents an analysis of time-series for hydrometeorological conditions determining the behavior of the natural environment in the South Baltic coastal zone of Poland. The analysis is based on monthly data for average air temperature, total atmospheric precipitation, and average sea level during the 50-year period from 1966–2015 for three coastal stations in Hel, Ustka, and Świnoujście. Time decomposition of these hydrometeorological conditions and formulation of short-term forecasts were carried out using ARIMA modelling. This study identifies the seasonal and non-seasonal parameters that determine both current and future hydrometeorological conditions. Moreover, it indicates the spatial differences among features of the analyzed time-series, estimated parameters of the selected models, and forecasts. The ARIMA models used for the Polish Baltic coastal zone are somewhat spatially homogenous. This is especially true of the models for average monthly air temperature, which are identical across the entire coastal zone (2,0,1)(2,1,0)12. Very similar are the models for average monthly sea level across the central and west coast (1,0,0)(1,1,0)12. The model for the east coast, however, was determined to be slightly different (2,0,2)(2,1,0)12. In contrast to those for air temperature and sea level, the models used for atmospheric precipitation were different for each site. Among the parameters modelled, the effect of AR(p) processes was greater than that of MA(q) processes. The monthly models for Ustka are an example of this: average air temperature (2,0,1)(2,1,0)12, atmospheric precipitation (0,0,3)(2,1,0)12, and average sea level (1,0,0)(1,1,0)12. Time decomposition of extreme hydrometeorological conditions has an important utilitarian significance. The climate of the Polish Baltic coastal zone is getting warmer, the sea level is rising, and the frequency of extreme hydrometeorological events is increasing. Time decomposition of hydrometeorological conditions based on monthly data did not reveal long-term trends. In the last half-century, hydrometeorological conditions have been conducive to erosion of coastal dunes and cliffs. These factors determine changes in the natural environment and limit the development potential of the coastal zone. The time decomposition, modelling, and forecasting of hydrometeorological conditions are thus very important for many areas of human activity, especially those related to management, protection, and development of the coast." @default.
• W2912155001 created "2019-02-21" @default.
• W2912155001 creator A5033100951 @default.
• W2912155001 creator A5081532522 @default.
• W2912155001 date "2019-01-29" @default.
• W2912155001 modified "2023-10-12" @default.
• W2912155001 title "Time Decomposition and Short-Term Forecasting of Hydrometeorological Conditions in the South Baltic Coastal Zone of Poland" @default.
• W2912155001 cites W1984061847 @default.
• W2912155001 cites W1986374422 @default.
• W2912155001 cites W1987376992 @default.
• W2912155001 cites W1992866626 @default.
• W2912155001 cites W2007485939 @default.
• W2912155001 cites W2008007961 @default.
• W2912155001 cites W2013376406 @default.
• W2912155001 cites W2014397586 @default.
• W2912155001 cites W2024112585 @default.
• W2912155001 cites W2046794274 @default.
• W2912155001 cites W2056237915 @default.
• W2912155001 cites W2065363804 @default.
• W2912155001 cites W2069570507 @default.
• W2912155001 cites W2106766562 @default.
• W2912155001 cites W2142635246 @default.
• W2912155001 cites W2151482884 @default.
• W2912155001 cites W2152269072 @default.
• W2912155001 cites W2155579932 @default.
• W2912155001 cites W2331764059 @default.
• W2912155001 cites W2344249856 @default.
• W2912155001 cites W2410521494 @default.
• W2912155001 cites W2565104007 @default.
• W2912155001 cites W2606950124 @default.
• W2912155001 cites W2694214741 @default.
• W2912155001 cites W2727610403 @default.
• W2912155001 cites W2785525000 @default.
• W2912155001 cites W2786511986 @default.
• W2912155001 cites W2804416042 @default.
• W2912155001 cites W2805252085 @default.
• W2912155001 cites W2847020481 @default.
• W2912155001 cites W2887248715 @default.
• W2912155001 cites W2893370393 @default.
• W2912155001 cites W2893537734 @default.
• W2912155001 cites W2893617732 @default.
• W2912155001 cites W2996493790 @default.
• W2912155001 cites W3121144236 @default.
• W2912155001 cites W4246587917 @default.
• W2912155001 cites W4318833898 @default.
• W2912155001 doi "https://doi.org/10.3390/geosciences9020068" @default.
• W2912155001 hasPublicationYear "2019" @default.
• W2912155001 type Work @default.
• W2912155001 sameAs 2912155001 @default.
• W2912155001 citedByCount "10" @default.
• W2912155001 countsByYear W29121550012019 @default.
• W2912155001 countsByYear W29121550012020 @default.
• W2912155001 countsByYear W29121550012021 @default.
• W2912155001 countsByYear W29121550012022 @default.
• W2912155001 countsByYear W29121550012023 @default.
• W2912155001 crossrefType "journal-article" @default.
• W2912155001 hasAuthorship W2912155001A5033100951 @default.
• W2912155001 hasAuthorship W2912155001A5081532522 @default.
• W2912155001 hasBestOaLocation W29121550011 @default.
• W2912155001 hasConcept C100725284 @default.
• W2912155001 hasConcept C105795698 @default.
• W2912155001 hasConcept C107054158 @default.
• W2912155001 hasConcept C111368507 @default.
• W2912155001 hasConcept C121332964 @default.
• W2912155001 hasConcept C127313418 @default.
• W2912155001 hasConcept C148043351 @default.
• W2912155001 hasConcept C151406439 @default.
• W2912155001 hasConcept C153294291 @default.
• W2912155001 hasConcept C205649164 @default.
• W2912155001 hasConcept C24338571 @default.
• W2912155001 hasConcept C2983363897 @default.
• W2912155001 hasConcept C2986433049 @default.
• W2912155001 hasConcept C33923547 @default.
• W2912155001 hasConcept C39432304 @default.
• W2912155001 hasConcept C49204034 @default.
• W2912155001 hasConcept C61797465 @default.
• W2912155001 hasConcept C62520636 @default.
• W2912155001 hasConcept C91586092 @default.
• W2912155001 hasConceptScore W2912155001C100725284 @default.
• W2912155001 hasConceptScore W2912155001C105795698 @default.
• W2912155001 hasConceptScore W2912155001C107054158 @default.
• W2912155001 hasConceptScore W2912155001C111368507 @default.
• W2912155001 hasConceptScore W2912155001C121332964 @default.
• W2912155001 hasConceptScore W2912155001C127313418 @default.
• W2912155001 hasConceptScore W2912155001C148043351 @default.
• W2912155001 hasConceptScore W2912155001C151406439 @default.
• W2912155001 hasConceptScore W2912155001C153294291 @default.
• W2912155001 hasConceptScore W2912155001C205649164 @default.
• W2912155001 hasConceptScore W2912155001C24338571 @default.
• W2912155001 hasConceptScore W2912155001C2983363897 @default.
• W2912155001 hasConceptScore W2912155001C2986433049 @default.
• W2912155001 hasConceptScore W2912155001C33923547 @default.
• W2912155001 hasConceptScore W2912155001C39432304 @default.
• W2912155001 hasConceptScore W2912155001C49204034 @default.
• W2912155001 hasConceptScore W2912155001C61797465 @default.
• W2912155001 hasConceptScore W2912155001C62520636 @default.
• W2912155001 hasConceptScore W2912155001C91586092 @default.
• W2912155001 hasIssue "2" @default.

• next