The paper presents critical remarks on reconstruction by Makos and Nowacki (2009). The authors worked out a model of ice-surface geometry and equilibrium line altitude (ELA) of glacier which existed in the Białka Valley system (High Tatra Mts.) during the Last Glacial Maximum (LGM), utilizing mapped trimlines in accumulation areas and literature data about glacier extent in ablation areas. Some palaeoclimate implications from this study indicate LGM-modern temperature amplitude ca 5.5grade C from ELA depression and prevailing southern atmospheric circulation pattern during the LGM in the Tatra Mts. The reconstruction does not comprise the whole former glacier system of the valley and therefore the use of arbitrary assumed accumulation area ...
The paper presents examination of views on number and age of glaciations in the Tatra Mts. and a new...
Tato diplomová práce se zabývá glaciálními kary Vysokých Tater - z pohledu jejich morfometrických ch...
Past fluctuations of tropical and sub-tropical glaciers provide important palaeoclimate proxies for ...
This paper is an answer to the polemical article Critical remarks on reconstruction of surface geome...
A reconstruction of the last glacial maximum (LGM) ice surface geometry in the Polish High Tatra Mts...
The Tatra Mountains extend along the border between Slovakia and Poland in the Western Carpathians. ...
An empirical glacio-climatic relation (Ohmura et al., 1992) and meteorological data (temperature and...
Be-10 exposure age chronology of the last glaciation was established in a key area at the southern s...
In the Western Carpathians, clear evidence of the Pleistocene glaciations only occurs in two mountai...
Glacier-based reconstructions of Equilibrium Line Altitudes (ELAs) are important to understand chang...
International audience\textcopyright 2016 Elsevier Ltd.Deglaciation chronology of the Bystra catchme...
Like in the High Tatras, a well-developed set of glacial and periglacial landforms marks successive ...
Lodowce maksimum ostatniego zlodowacenia oraz rozmieszczenie starszych osadów glacjalnych Mapa i b...
International audienceRelict rock glaciers are well-preserved features of high-elevated valleys in t...
Kartowanie form i osadów glacjalnych oraz rekonstrukcja geometrii paleolodowców stanowią podstawowe ...
The paper presents examination of views on number and age of glaciations in the Tatra Mts. and a new...
Tato diplomová práce se zabývá glaciálními kary Vysokých Tater - z pohledu jejich morfometrických ch...
Past fluctuations of tropical and sub-tropical glaciers provide important palaeoclimate proxies for ...
This paper is an answer to the polemical article Critical remarks on reconstruction of surface geome...
A reconstruction of the last glacial maximum (LGM) ice surface geometry in the Polish High Tatra Mts...
The Tatra Mountains extend along the border between Slovakia and Poland in the Western Carpathians. ...
An empirical glacio-climatic relation (Ohmura et al., 1992) and meteorological data (temperature and...
Be-10 exposure age chronology of the last glaciation was established in a key area at the southern s...
In the Western Carpathians, clear evidence of the Pleistocene glaciations only occurs in two mountai...
Glacier-based reconstructions of Equilibrium Line Altitudes (ELAs) are important to understand chang...
International audience\textcopyright 2016 Elsevier Ltd.Deglaciation chronology of the Bystra catchme...
Like in the High Tatras, a well-developed set of glacial and periglacial landforms marks successive ...
Lodowce maksimum ostatniego zlodowacenia oraz rozmieszczenie starszych osadów glacjalnych Mapa i b...
International audienceRelict rock glaciers are well-preserved features of high-elevated valleys in t...
Kartowanie form i osadów glacjalnych oraz rekonstrukcja geometrii paleolodowców stanowią podstawowe ...
The paper presents examination of views on number and age of glaciations in the Tatra Mts. and a new...
Tato diplomová práce se zabývá glaciálními kary Vysokých Tater - z pohledu jejich morfometrických ch...
Past fluctuations of tropical and sub-tropical glaciers provide important palaeoclimate proxies for ...