Zobrazeno 1 - 10
of 17
pro vyhledávání: '"Lequan Chi"'
Publikováno v:
Geophysical Research Letters, Vol 50, Iss 9, Pp n/a-n/a (2023)
Abstract The relationship between Gulf Stream (GS) transport and coastal sea level is investigated using monthly GS transport between 1993 and 2019 at Florida Straits and 10 altimeter tracks. The results show that GS transport decorrelates quickly al
Externí odkaz:
https://doaj.org/article/fc3873851e7c416ca00bbe9fab0ab1ee
Publikováno v:
Geophysical Research Letters, Vol 46, Iss 15, Pp 8943-8951 (2019)
Abstract Downstream of Cape Hatteras, the Gulf Stream (GS) is bounded to the north by a sharp temperature front known as the North Wall (NW). Previous studies have generally assumed that variations of the NW and GS are equivalent. Using satellite sea
Externí odkaz:
https://doaj.org/article/abece52b163e4ccfa91b116db09a2312
The relationship between Gulf Stream (GS) transport and coastal sea level is investigated using monthly GS transport between 1993–2019 at Florida Straits and ten altimeter tracks. The results show ...
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a4d56050870e0004b589a00c599bf133
https://doi.org/10.1002/essoar.10508225.1
https://doi.org/10.1002/essoar.10508225.1
Publikováno v:
Journal of Coastal Research. 37
Swanson, R.L.; Giglio, K.W., and Chi, L., 2021. Restoring a degraded, sentinel New England salt marsh to mid-20th century conditions (Flax Pond, New York, U.S.A.). Journal of Coastal Research, 37(5), 993–1011. Coconut Creek (Florida), ISSN 0749-020
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f1369db8652a74a78dff73922b2a5b20
https://doi.org/10.2112/jcoastres-d-20-00043.1
https://doi.org/10.2112/jcoastres-d-20-00043.1
Publikováno v:
Journal of Physical Oceanography.
Previous work to find an association between variations of annually averaged Florida Current transport and the North Atlantic Oscillation (NAO) have yielded negative results (Meinen et al. 2010). Here we show that Florida current in winter is impacte
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b9f9863bdd399b71f73531ad19d4f0df
https://doi.org/10.1175/jpo-d-20-0108.1
https://doi.org/10.1175/jpo-d-20-0108.1
Publikováno v:
Geophysical Research Letters. 48
The Gulf Stream is expected to slow and shift poleward over the next century due to climate change. We investigate whether such changes are already observable in the altimetric record (1993–2018) u...
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::796f1b789f7b8cf28aebc027880446b7
https://doi.org/10.1029/2021gl093113
https://doi.org/10.1029/2021gl093113
Publikováno v:
Acta Oceanologica Sinica. 38:20-30
Numerical simulations based on a high-resolution three-dimensional MIT general circulation model (MITgcm) using realistic topography and tidal forcing are conducted to investigate the generation and propagation of the so-called type-a waves (large-am
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::01aefa17806b72fe9dc7c6c35b017a96
https://doi.org/10.1007/s13131-019-1495-2
https://doi.org/10.1007/s13131-019-1495-2
Publikováno v:
Journal of Physical Oceanography. 49:2731-2734
The path of the Gulf Stream as it leaves the continental shelf near Cape Hatteras is marked by a sharp gradient in ocean temperature known as the North Wall. The latitude location of the Gulf Stream North Wall (GSNW) has previously been estimated by
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0a484cb8024f740ff90328b05ce0b105
https://doi.org/10.1175/jpo-d-19-0096.1
https://doi.org/10.1175/jpo-d-19-0096.1
Publikováno v:
Geophysical Research Letters. 46:8943-8951
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4857c0ede02bfaa45013f08b1b49574c
https://doi.org/10.1029/2019gl083775
https://doi.org/10.1029/2019gl083775
Publikováno v:
Journal of Climate. 32:1235-1249
The Gulf Stream is bounded to the north by a strong temperature front known as the North Wall. The North Wall is subject to variability on a wide range of temporal and spatial scales—on interannual time scales, the dominant mode of variability is a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c9cc5602b7975d9dd86866da9512d3bc
https://doi.org/10.1175/jcli-d-18-0212.1
https://doi.org/10.1175/jcli-d-18-0212.1