Zobrazeno 1 - 10
of 102
pro vyhledávání: '"Jong-Kuk Choi"'
Publikováno v:
Remote Sensing, Vol 16, Iss 12, p 2111 (2024)
During the summer, substantial freshwater discharge from the Changjiang River into the East China Sea (ECS) results in extensive low-salinity water (LSW) plumes that significantly affect regions along the southern Korean Peninsula and near Jeju Islan
Externí odkaz:
https://doaj.org/article/81b9537915c44a418061e45a43c7948a
Autor:
Young Baek Son, Jong-Kuk Choi
Publikováno v:
Frontiers in Marine Science, Vol 9 (2022)
The Changjiang River loads freshwater into the East China Sea (ECS) and the Yellow Sea (YS). A low-salinity plume known as Changjiang Diluted Water (CDW) is formed by mixing with saline ambient waters; it disperses toward Jeju Island and the East/Jap
Externí odkaz:
https://doaj.org/article/84b1539c588f415abae097792e9c752b
Autor:
Deuk Jae Hwang, Robert Frouin, Jing Tan, Jae-Hyun Ahn, Jong-Kuk Choi, Jeong-Eon Moon, Joo-Hyung Ryu
Publikováno v:
Frontiers in Marine Science, Vol 9 (2022)
Photosynthetically available radiation (PAR) reaching the ocean surface controls phytoplankton growth, primary productivity, and evolution within marine ecosystems. Therefore, accurate daily PAR estimates are important for a broad range of marine bio
Externí odkaz:
https://doaj.org/article/e9c19a1247af466ca79e43e2d9366e01
Publikováno v:
Remote Sensing, Vol 15, Iss 8, p 2124 (2023)
In remote sensing of the ocean color, in particular, in coarse-resolution global model simulations, atmospheric trace gases including water vapor are generally treated as auxiliary data, which create uncertainties in atmospheric correction. The secon
Externí odkaz:
https://doaj.org/article/13fbc0fe23c542edb23bf1d506443d76
Publikováno v:
Geo Data, Vol 2, Iss 2, Pp 26-35 (2020)
The Hwangdo tidal flat has been subjected to local hydrodynamic changes caused by the construction of seawalls and bridges, which are changing the distribution of sediments and topographic characteristics. These changes would affect the sedimentary e
Externí odkaz:
https://doaj.org/article/1f41135350304e908861c362d427ab47
Publikováno v:
Geo Data, Vol 2, Iss 2, Pp 5-13 (2020)
Remote sensing reflectance (Rrs) is a fundamental data of ocean color remote sensing that is used as an input data for algorithm development. In this study, the Rrs spectra acquired from the coast of Korea and California, on the opposite side of the
Externí odkaz:
https://doaj.org/article/0f40473c579a4377afd121f56ad4c609
Autor:
Jeong-Eon Moon, Tai-Hyun Han, Kwang-Seok Kim, Deuk-Jae Hwang, Jae-Hyun Ahn, Jong-Kuk Choi, Joo-Hyung Ryu, Young-Je Park
Publikováno v:
Geo Data, Vol 1, Iss 1, Pp 29-37 (2019)
The chlorophyll and total suspended materials concentrations and remote sensing reflectance data were observed for red tides occurring every summer in waters around the Korean Peninsula. In observation area and date, the field survey were performed (
Externí odkaz:
https://doaj.org/article/591a7b599f3c4d588e43ad4e43460a85
Publikováno v:
Remote Sensing, Vol 14, Iss 1, p 72 (2021)
The first geostationary ocean color data from the Geostationary Ocean Color Imager (GOCI) onboard the Communication, Ocean, and Meteorological Satellite (COMS) have been accumulating for more than ten years from 2010. This study performs a multi-year
Externí odkaz:
https://doaj.org/article/1c5e02d904a8485aa5daa7487b163e18
Publikováno v:
Remote Sensing, Vol 13, Iss 24, p 5169 (2021)
Coastal zones are very dynamic natural systems that experience short-term and long-term morphological changes. Their highly dynamic behavior requires frequent monitoring. Tidal flat topography for a large spatial coverage has been generated mainly by
Externí odkaz:
https://doaj.org/article/7c9ada4527514073be09230b34bcff19
Publikováno v:
Remote Sensing, Vol 13, Iss 14, p 2676 (2021)
During the summer season, low-salinity water (LSW) inputs from the Changjiang River are observed as filamentous or lens-like features in the East China Sea. Sea surface salinity (SSS) is an important factor in ocean science, and is used to estimate o
Externí odkaz:
https://doaj.org/article/5d6e41c3246247298fa3f3cff4d0892c