Post-Little Ice Age development of coast in the locality of
Kapp Napier, central Spitsbergen, Svalbard archipelago

J 2020

Post-Little Ice Age development of coast in the locality of Kapp Napier, central Spitsbergen, Svalbard archipelago

KAVAN, Jan

Základní údaje

Originální název

Post-Little Ice Age development of coast in the locality of Kapp Napier, central Spitsbergen, Svalbard archipelago

Autoři

KAVAN, Jan

Vydání

Marine Geodesy, PHILADELPHIA, TAYLOR & FRANCIS INC, 2020, 0149-0419

Další údaje

Jazyk

angličtina

Typ výsledku

Článek v odborném periodiku

Obor

10502 Oceanography

Stát vydavatele

Spojené státy

Utajení

není předmětem státního či obchodního tajemství

Odkazy

URL

Impakt faktor

Impact factor: 1.667

Označené pro přenos do RIV

Ano

Kód RIV

RIV/00216224:14310/20:00115344

Organizační jednotka

Přírodovědecká fakulta

Klíčová slova anglicky

Climate change; coast evolution; glacier; historic photographs; Svalbard

Štítky

14315030, rivok

Příznaky

Mezinárodní význam, Recenzováno

Změněno: 5. 1. 2021 22:48, Mgr. Marie Novosadová Šípková, DiS.

Anotace

V originále

Changes in the position of the shore in the vicinity of Kapp Napier in central Svalbard was described. The overall advance of the shore was probably related to high input of the sediment material originating from erosion of the coastal areas south of the Kapp Napier locality and high input of material from adjacent glacifluvial system of Nordenski?ld glacier with its marginal water streams. Fast evolution of glacier retreat related processes after the Little Ice Age was a secondary driver of the dynamic changes in the central Svalbard coastal areas especially in the first half of the 20th century. The highly dynamic longshore currents in the area altogether with still ongoing glacio-isostatic uplift played an important role in the process as well. The most active parts of the shore experienced advance of almost 100 m since 1908 to 2009. On the other hand, a small part of the coast retreated of about 20 m. Most of the study area experienced aggradation (65%), 30% of the coast was stable and about 5% of the coast has undergone minor retreat. The maximum aggradation rate of 0.96?m/year corresponds well with similar sites in the vicinity.

Návaznosti

LM2015078, projekt VaV

Název: Česká polární výzkumná infrastruktura (Akronym: CzechPolar2)

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

MUNI/A/1251/2017, interní kód MU

Název: Integrovaný výzkum environmentálních změn v krajinné sféře Země III

Investor: Masarykova univerzita, Integrovaný výzkum environmentálních změn v krajinné sféře Země III, DO R. 2020_Kategorie A - Specifický výzkum - Studentské výzkumné projekty

Citovat

KAVAN, Jan. Post-Little Ice Age development of coast in the locality of Kapp Napier, central Spitsbergen, Svalbard archipelago. Marine Geodesy. PHILADELPHIA: TAYLOR & FRANCIS INC, 2020, roč. 43, č. 3, s. 234-247. ISSN 0149-0419. Dostupné z: https://doi.org/10.1080/01490419.2019.1674429.

@article{1625656,
   author = {Kavan, Jan},
   article_location = {PHILADELPHIA},
   article_number = {3},
   doi = {https://doi.org/10.1080/01490419.2019.1674429},
   keywords = {Climate change; coast evolution; glacier; historic photographs; Svalbard},
   language = {eng},
   issn = {0149-0419},
   journal = {Marine Geodesy},
   title = {Post-Little Ice Age development of coast in the locality of Kapp Napier, central Spitsbergen, Svalbard archipelago},
   url = {https://www.tandfonline.com/doi/abs/10.1080/01490419.2019.1674429},
   volume = {43},
   year = {2020}
}

TY  - JOUR
ID  - 1625656
AU  - Kavan, Jan
PY  - 2020
TI  - Post-Little Ice Age development of coast in the locality of Kapp Napier, central Spitsbergen, Svalbard archipelago
JF  - Marine Geodesy
VL  - 43
IS  - 3
SP  - 234-247
EP  - 234-247
PB  - TAYLOR & FRANCIS INC
SN  - 01490419
KW  - Climate change
KW  - coast evolution
KW  - glacier
KW  - historic photographs
KW  - Svalbard
UR  - https://www.tandfonline.com/doi/abs/10.1080/01490419.2019.1674429
L2  - https://www.tandfonline.com/doi/abs/10.1080/01490419.2019.1674429
N2  - Changes in the position of the shore in the vicinity of Kapp Napier in central Svalbard was described. The overall advance of the shore was probably related to high input of the sediment material originating from erosion of the coastal areas south of the Kapp Napier locality and high input of material from adjacent glacifluvial system of Nordenski?ld glacier with its marginal water streams. Fast evolution of glacier retreat related processes after the Little Ice Age was a secondary driver of the dynamic changes in the central Svalbard coastal areas especially in the first half of the 20th century. The highly dynamic longshore currents in the area altogether with still ongoing glacio-isostatic uplift played an important role in the process as well. The most active parts of the shore experienced advance of almost 100 m since 1908 to 2009. On the other hand, a small part of the coast retreated of about 20 m. Most of the study area experienced aggradation (65%), 30% of the coast was stable and about 5% of the coast has undergone minor retreat. The maximum aggradation rate of 0.96?m/year corresponds well with similar sites in the vicinity.
ER  -

KAVAN, Jan. Post-Little Ice Age development of coast in the locality of Kapp Napier, central Spitsbergen, Svalbard archipelago. \textit{Marine Geodesy}. PHILADELPHIA: TAYLOR \&{} FRANCIS INC, 2020, roč.~43, č.~3, s.~234-247. ISSN~0149-0419. Dostupné z: https://doi.org/10.1080/01490419.2019.1674429.

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