FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4297383368> ?p ?o ?g. }

• W4297383368 endingPage "1375" @default.
• W4297383368 startingPage "1351" @default.
• W4297383368 abstract "Abstract. Ocean mass change is one of the main drivers of present-day sea-level change (SLC). Also known as barystatic SLC, ocean mass change is caused by the exchange of freshwater between the land and the ocean, such as melting of continental ice from glaciers and ice sheets, and variations in land water storage. While many studies have quantified the present-day barystatic contribution to global mean SLC, fewer works have looked into regional changes. This study provides an analysis of regional patterns of contemporary mass redistribution associated with barystatic SLC since 1993 (the satellite altimetry era), with a focus on the uncertainty budget. We consider three types of uncertainties: intrinsic (the uncertainty from the data/model itself), temporal (related to the temporal variability in the time series) and spatial–structural (related to the spatial distribution of the mass change sources). Regional patterns (fingerprints) of barystatic SLC are computed from a range of estimates of the individual freshwater sources and used to analyze the different types of uncertainty. Combining all contributions, we find that regional sea-level trends range from −0.4 to 3.3 mm yr−1 for 2003–2016 and from −0.3 to 2.6 mm yr−1 for 1993–2016, considering the 5–95th percentile range across all grid points and depending on the choice of dataset. When all types of uncertainties from all contributions are combined, the total barystatic uncertainties regionally range from 0.6 to 1.3 mm yr−1 for 2003–2016 and from 0.4 to 0.8 mm yr−1 for 1993–2016, also depending on the dataset choice. We find that the temporal uncertainty dominates the budget, responsible on average for 65 % of the total uncertainty, followed by the spatial–structural and intrinsic uncertainties, which contribute on average 16 % and 18 %, respectively. The main source of uncertainty is the temporal uncertainty from the land water storage contribution, which is responsible for 35 %–60 % of the total uncertainty, depending on the region of interest. Another important contribution comes from the spatial–structural uncertainty from Antarctica and land water storage, which shows that different locations of mass change can lead to trend deviations larger than 20 %. As the barystatic SLC contribution and its uncertainty vary significantly from region to region, better insights into regional SLC are important for local management and adaptation planning." @default.
• W4297383368 created "2022-09-28" @default.
• W4297383368 creator A5013539173 @default.
• W4297383368 creator A5041541652 @default.
• W4297383368 creator A5057613319 @default.
• W4297383368 creator A5090593125 @default.
• W4297383368 date "2022-09-27" @default.
• W4297383368 modified "2023-10-17" @default.
• W4297383368 title "Trends and uncertainties of mass-driven sea-level change in the satellite altimetry era" @default.
• W4297383368 cites W1532228020 @default.
• W4297383368 cites W1588827410 @default.
• W4297383368 cites W1951817746 @default.
• W4297383368 cites W1984430226 @default.
• W4297383368 cites W1992519610 @default.
• W4297383368 cites W1997722977 @default.
• W4297383368 cites W2006900639 @default.
• W4297383368 cites W2007815508 @default.
• W4297383368 cites W2028200333 @default.
• W4297383368 cites W2029748484 @default.
• W4297383368 cites W2062221814 @default.
• W4297383368 cites W2072613263 @default.
• W4297383368 cites W2076202396 @default.
• W4297383368 cites W2094988303 @default.
• W4297383368 cites W2102065044 @default.
• W4297383368 cites W2103751670 @default.
• W4297383368 cites W2119805620 @default.
• W4297383368 cites W2127914213 @default.
• W4297383368 cites W2128974637 @default.
• W4297383368 cites W2140888393 @default.
• W4297383368 cites W2142446883 @default.
• W4297383368 cites W2142635246 @default.
• W4297383368 cites W2143784106 @default.
• W4297383368 cites W2147988117 @default.
• W4297383368 cites W2150948381 @default.
• W4297383368 cites W2151329188 @default.
• W4297383368 cites W2154207321 @default.
• W4297383368 cites W2167421857 @default.
• W4297383368 cites W2168175751 @default.
• W4297383368 cites W2168407872 @default.
• W4297383368 cites W2272911618 @default.
• W4297383368 cites W2320730453 @default.
• W4297383368 cites W2505756961 @default.
• W4297383368 cites W2512174018 @default.
• W4297383368 cites W2520852046 @default.
• W4297383368 cites W2523841373 @default.
• W4297383368 cites W2536819440 @default.
• W4297383368 cites W2590402896 @default.
• W4297383368 cites W2606431300 @default.
• W4297383368 cites W2749109638 @default.
• W4297383368 cites W2768939228 @default.
• W4297383368 cites W2769185573 @default.
• W4297383368 cites W2772564114 @default.
• W4297383368 cites W2790934709 @default.
• W4297383368 cites W2791275538 @default.
• W4297383368 cites W2791684036 @default.
• W4297383368 cites W2801080873 @default.
• W4297383368 cites W2810491782 @default.
• W4297383368 cites W2883436694 @default.
• W4297383368 cites W2908740848 @default.
• W4297383368 cites W2909402432 @default.
• W4297383368 cites W2912635068 @default.
• W4297383368 cites W2913304119 @default.
• W4297383368 cites W2914401989 @default.
• W4297383368 cites W2934984619 @default.
• W4297383368 cites W2938442499 @default.
• W4297383368 cites W2943222986 @default.
• W4297383368 cites W2946106424 @default.
• W4297383368 cites W2969008563 @default.
• W4297383368 cites W2995568124 @default.
• W4297383368 cites W3007551985 @default.
• W4297383368 cites W3026223029 @default.
• W4297383368 cites W3028476923 @default.
• W4297383368 cites W3038601193 @default.
• W4297383368 cites W3071221217 @default.
• W4297383368 cites W3089079348 @default.
• W4297383368 cites W3111474552 @default.
• W4297383368 cites W3118407704 @default.
• W4297383368 cites W3118477507 @default.
• W4297383368 cites W3145149478 @default.
• W4297383368 cites W3158099307 @default.
• W4297383368 cites W3162991635 @default.
• W4297383368 cites W3177416308 @default.
• W4297383368 cites W3208979220 @default.
• W4297383368 cites W4210320361 @default.
• W4297383368 cites W4210654828 @default.
• W4297383368 cites W4210662379 @default.
• W4297383368 cites W4244706146 @default.
• W4297383368 doi "https://doi.org/10.5194/esd-13-1351-2022" @default.
• W4297383368 hasPublicationYear "2022" @default.
• W4297383368 type Work @default.
• W4297383368 citedByCount "2" @default.
• W4297383368 countsByYear W42973833682023 @default.
• W4297383368 crossrefType "journal-article" @default.
• W4297383368 hasAuthorship W4297383368A5013539173 @default.
• W4297383368 hasAuthorship W4297383368A5041541652 @default.
• W4297383368 hasAuthorship W4297383368A5057613319 @default.
• W4297383368 hasAuthorship W4297383368A5090593125 @default.
• W4297383368 hasBestOaLocation W42973833681 @default.

• next