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Wyświetlanie 1-2 z 2
Tytuł:
Rola instytutów badawczych we wsparciu działań adaptacyjnych do zmian klimatu
The actions of research institutes to support adaptation to climate change
Autorzy:
Granoszewski, Wojciech
Kowalczyk, Agnieszka
Ploch, Izabela
Rubinkiewicz, Jacek
Woźnicka, Małgorzata
Kępińska-Kasprzak, Małgorzata
Limanówka, Danuta
Doktor, Radosław
Struzik, Piotr
Dubel, Anna
Skotak, Krzysztof
Hajto, Małgorzata
Kozyra, Jerzy
Pudełko, Rafał
Żyłowska, Katarzyna
Jędrejek, Anna
Łopatka, Artur
Jadczyszyn, Jan
Nieróbca, Anna
Doroszewski, Andrzej
Barszczewska, Marta
Powiązania:
https://bibliotekanauki.pl/articles/2076003.pdf
Data publikacji:
2020
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
zmiany klimatu
systemy monitorowania
warunki meteorologiczne
powierzchnia wody
wody gruntowe
osuwiska
wybrzeże
susza rolnicza
dane paleoklimatyczne
ocena ekonomiczna
skutki zmian klimatu
ryzyko katastrof
climate change
monitoring systems
meteorological conditions
surface water
groundwater
landslides
seacoast
agricultural drought
palaeoclimate data
economic assessment
climate change impacts
disaster risk reduction
Opis:
A crucial part of every adaptation planning and disaster risk reduction is estimation of vulnerable areas and risk in the future. Only a well-developed monitoring system could bring valuable information to create possible scenarios to set up adaptation plans. Monitoring systems of meteorological conditions, surface water, groundwater, landslides, seacoast, agricultural drought as well as their standards and methodologies, are crucial for establishing an effective warning system of every country, and thus are the subject of research conducted by national institutes. Therefore, the conditions of this national research (getting trained staff, equipment etc.) is essential to provide reliable information for a national adaptation plan and for economic assessment of climate change impacts. Poland has significant experiences in monitoring systems, data collecting and visualizing, as well as in the development of scenarios and risk maps. Methodologies and capacity building, necessary for their use, along with experiences and lessons, learned to get valuable information for disaster risk reduction, were presented by the authors from the research during the 24th session of the Conference of the Parties to the United Nations Framework Convention on Climate Change (COP 24) in Katowice (December 2018). The presentation contributed to the global adaptation process through experience sharing that is important for the relevant research conducted in the least developed countries.
Źródło:
Przegląd Geologiczny; 2020, 68, 1; 25--44
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
The mineralogical record of the Early Toarcian stepwise climate changes and other environmental variations (Ciechocinek Formation, Polish Basin)
Autorzy:
Brański, P.
Powiązania:
https://bibliotekanauki.pl/articles/2061010.pdf
Data publikacji:
2012
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
clay minerals
bulk rock data
warming event
palaeoclimate
Ciechocinek Formation
Early Toarcian
Polish Basin
minerały ilaste
okres ocieplenia
Formacja Ciechocińska
wczesny toark
basen polski
Opis:
After the cooling episode of the Late Pliensbachian, a major oceanic anoxic event occurred during the prominent warming event of the Early Toarcian (183 Myr; Early Jurassic). In this paper, new mineralogical and geochemical data (XRD, XRF, SEM, and TOC) measured on four cores from the Polish Basin are presented in order to document the regional impacts of these disturbances at a high sampling resolution. The results show that the clay mineral assemblages (<2 μm fraction) and vertical variations in kaolinite content are generally similar basin-wide and were controlled by the intensity of chemical weathering and climate changes. However, sea-level changes and variations in terrigenous supply are reflected in the bulk rock data. The spatial variability in clay mineral proportions may also be influenced by the distance from shoreline and the lithology of source areas. Generally, the clay minerals from the Polish Basin confirm the stepped nature of the Early Toarcian warming event. After a predominance of illite in the lower part of the Ciechocinek Fm., which suggests a temperate climate in the early tenuicostatum Zone, rises in kaolinite in the middle part of the Ciechocinek Fm. indicate a stronger weathering rate and high rainfall due to the onset of the warming event in the late tenuicostatum Zone. Importantly, the initial phase of climate change recorded by clay minerals seems to slightly precede the first step of the negative carbon isotope excursion ascribed to massive greenhouse gas releases.
Źródło:
Volumina Jurassica; 2012, 10, 1; 1--24
1896-7876
1731-3708
Pojawia się w:
Volumina Jurassica
Dostawca treści:
Biblioteka Nauki
Artykuł
    Wyświetlanie 1-2 z 2

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