Is the positive mass balance of north-eastern Antarctic
Peninsula glaciers persistent after 2015?

a 2018

Is the positive mass balance of north-eastern Antarctic Peninsula glaciers persistent after 2015?

LÁSKA, Kamil, Zbyněk ENGEL, Daniel NÝVLT, Zdeněk STACHOŇ, Jan KAVAN et. al.

Základní údaje

Originální název

Is the positive mass balance of north-eastern Antarctic Peninsula glaciers persistent after 2015?

Autoři

LÁSKA, Kamil, Zbyněk ENGEL, Daniel NÝVLT, Zdeněk STACHOŇ, Jan KAVAN, Jana SMOLÍKOVÁ, Radim STUCHLÍK, Stefan LIPPL a Matthias BRAUN

Vydání

European Geosciences Union General Assembly 2018, 2018

Další údaje

Jazyk

angličtina

Typ výsledku

Konferenční abstrakt

Obor

10510 Climatic research

Stát vydavatele

Rakousko

Utajení

není předmětem státního či obchodního tajemství

Odkazy

Geophysical Research Abstracts, 2018

Organizační jednotka

Přírodovědecká fakulta

ISSN

Klíčová slova anglicky

Antarctica; James Ross Island;glacier;snow; ablation; accumulation; surface mass balance;

Příznaky

Mezinárodní význam, Recenzováno

Změněno: 5. 11. 2018 20:44, doc. Mgr. Daniel Nývlt, Ph.D.

Anotace

V originále

In this contribution, we tried to examine whether JRI glaciers could respond to climate variability in such a short time. We analysed annual mass balance changes of four dominant land-based glaciers in the northern part of JRI (Davies Dome, Whisky Glacier, Triangular Glacier, San Jose Glacier). The surface mass-balance changes were estimated based on ablation stakes and differential GNSS measurements, which were carried out over last two years (2015/16–2016/17). In addition, surface elevation changes were determined for this period and compared with digital elevation models (DEMs) created from available TanDEM-X scenes. The annual surface mass-balance was negative for the most of investigated glaciers in the 2015–17 period. One of the highest negative mass-balance was found for Whisky Glacier in 2015–16, when this glacier lost 0.36 m w.e. in average.

Návaznosti

CZ.02.1.01/0.0/0.0/16_013/0001708, interní kód MU
(Kód CEP: EF16_013/0001708)

Název: ECOPOLARIS - Změny ve struktuře a funkci součástí terestrických polárních ekosystémů (Akronym: ECOPOLARIS)

Investor: Ministerstvo školství, mládeže a tělovýchovy ČR, ECOPOLARIS - Změny ve struktuře a funkci součástí terestrických polárních ekosystémů, PO 1 Posilování kapacit pro kvalitní výzkum

GC16-14122J, projekt VaV

Název: Reakce ledovců na recentní klimatickou variabilitu v severovýchodní části Antarktického poloostrova

Investor: Grantová agentura ČR, Reakce ledovců na recentní klimatickou variabilitu v severovýchodní části Antarktického poloostrova

LM2015078, projekt VaV

Název: Česká polární výzkumná infrastruktura (Akronym: CzechPolar2)

Investor: Ministerstvo školství, mládeže a tělovýchovy ČR, Czech Polar Research Infrastructure

Citovat

LÁSKA, Kamil, Zbyněk ENGEL, Daniel NÝVLT, Zdeněk STACHOŇ, Jan KAVAN, Jana SMOLÍKOVÁ, Radim STUCHLÍK, Stefan LIPPL a Matthias BRAUN. Is the positive mass balance of north-eastern Antarctic Peninsula glaciers persistent after 2015? In European Geosciences Union General Assembly 2018. 2018. ISSN 1029-7006.

@proceedings{1439196,
   author = {Láska, Kamil and Engel, Zbyněk and Nývlt, Daniel and Stachoň, Zdeněk and Kavan, Jan and Smolíková, Jana and Stuchlík, Radim and Lippl, Stefan and Braun, Matthias},
   booktitle = {European Geosciences Union General Assembly 2018},
   keywords = {Antarctica; James Ross Island;glacier;snow; ablation; accumulation; surface mass balance;},
   language = {eng},
   title = {Is the positive mass balance of north-eastern Antarctic Peninsula glaciers persistent after 2015?},
   url = {https://www.egu2018.eu/},
   year = {2018}
}

TY  - CONF
ID  - 1439196
AU  - Láska, Kamil - Engel, Zbyněk - Nývlt, Daniel - Stachoň, Zdeněk - Kavan, Jan - Smolíková, Jana - Stuchlík, Radim - Lippl, Stefan - Braun, Matthias
PY  - 2018
TI  - Is the positive mass balance of north-eastern Antarctic Peninsula glaciers persistent after 2015?
KW  - Antarctica
KW  - James Ross Island;glacier;snow
KW  - ablation
KW  - accumulation
KW  - surface mass balance;
UR  - https://www.egu2018.eu/
L2  - https://www.egu2018.eu/
N2  - In this contribution, we tried to examine whether JRI glaciers could respond to climate variability in such a short time. We analysed annual mass balance changes of four dominant land-based glaciers in the northern part of JRI (Davies Dome, Whisky Glacier, Triangular Glacier, San Jose Glacier). The surface mass-balance changes were estimated based on ablation stakes and differential GNSS measurements, which were carried out over last two years (2015/16–2016/17). In addition, surface elevation changes were determined for this period and compared with digital elevation models (DEMs) created from available TanDEM-X scenes. The annual surface mass-balance was negative for the most of investigated glaciers in the 2015–17 period. One of the highest negative mass-balance was found for Whisky Glacier in 2015–16, when this glacier lost 0.36 m w.e. in average.
ER  -

LÁSKA, Kamil, Zbyněk ENGEL, Daniel NÝVLT, Zdeněk STACHOŇ, Jan KAVAN, Jana SMOLÍKOVÁ, Radim STUCHLÍK, Stefan LIPPL a Matthias BRAUN. Is the positive mass balance of north-eastern Antarctic Peninsula glaciers persistent after 2015? In \textit{European Geosciences Union General Assembly 2018}. 2018. ISSN~1029-7006.

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