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  • 1
    Publication Date: 2018-12-28
    Description: Hydrographic measurements from ships, autonomous profiling floats, and instrumented seals over the period 1986–2016 are used to examine the temporal variability in open-ocean convection in the Greenland Sea during winter. This process replenishes the deep ocean with oxygen and is central to maintaining its thermohaline properties. The deepest and densest mixed layers in the Greenland Sea were located within its cyclonic gyre and exhibited large interannual variability. Beginning in winter 1994, a transition to deeper (〉500 m) mixed layers took place. This resulted in the formation of a new, less dense class of intermediate water that has since become the main product of convection in the Greenland Sea. In the preceding winters, convection was limited to
    Print ISSN: 0022-3670
    Electronic ISSN: 1520-0485
    Topics: Geosciences , Physics
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  • 2
    Publication Date: 2019-08-21
    Description: Dense water masses transported southward along the east coast of Greenland in the East Greenland Current (EGC) form the largest contribution to the Denmark Strait Overflow. When exiting Denmark Strait these dense water masses sink to depth and feed the deep circulation in the North Atlantic. Based on one year of mooring observations upstream of Denmark Strait and historical hydrographic profiles between Fram Strait and Denmark Strait, we find that a large part (75%) of the overflow water (σθ ≥ 27.8 kg m−3) transported by the EGC is of Atlantic origin (potential temperature θ 〉 0°C). The along-stream changes in temperature of the Atlantic-origin Water are moderate north of 69°N at the northern end of Blosseville basin, but southward from this point the temperature decreases more rapidly. We hypothesize that this enhanced modification is related to the bifurcation of the EGC taking place close to 69°N into the shelfbreak EGC and the separated EGC. This is associated with enhanced eddy activity and strong water mass modification reducing the intermediate temperature and salinity maxima of the Atlantic-origin Water. During periods with a large (small) degree of modification the separated current is strong (weak). Output from a high-resolution numerical model supports our hypothesis and reveals that large eddy activity is associated with an offshore shift of the surface freshwater layer that characterizes the Greenland shelf. The intensity of the eddy activity regulates the density and the hydrographic properties of the Denmark Strait Overflow Water transported by the EGC system.
    Print ISSN: 0022-3670
    Electronic ISSN: 1520-0485
    Topics: Geosciences , Physics
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  • 3
    Publication Date: 2018-09-01
    Print ISSN: 2169-9275
    Electronic ISSN: 2169-9291
    Topics: Geosciences , Physics
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  • 4
    Publication Date: 2018-03-29
    Electronic ISSN: 2041-1723
    Topics: Biology , Chemistry and Pharmacology , Natural Sciences in General , Physics
    Published by Springer Nature
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  • 5
  • 6
    Publication Date: 2024-02-26
    Keywords: DATE/TIME; DEPTH, water; Event label; GLD; Glider; LATITUDE; LONGITUDE; North Atlantic; Pressure, water; Salinity; sg562_dive_001; sg562_dive_002; sg562_dive_003; sg562_dive_004; sg562_dive_005; sg562_dive_006; sg562_dive_007; sg562_dive_008; sg562_dive_009; sg562_dive_010; sg562_dive_011; sg562_dive_012; sg562_dive_013; sg562_dive_014; sg562_dive_015; sg562_dive_016; sg562_dive_017; sg562_dive_018; sg562_dive_019; sg562_dive_020; sg562_dive_021; sg562_dive_022; sg562_dive_023; sg562_dive_024; sg562_dive_025; sg562_dive_026; sg562_dive_027; sg562_dive_028; sg562_dive_029; sg562_dive_030; sg562_dive_031; sg562_dive_032; sg562_dive_033; sg562_dive_034; sg562_dive_035; sg562_dive_036; sg562_dive_037; sg562_dive_038; sg562_dive_039; sg562_dive_040; sg562_dive_041; sg562_dive_042; sg562_dive_043; sg562_dive_044; sg562_dive_045; sg562_dive_046; sg562_dive_047; sg562_dive_048; sg562_dive_049; sg562_dive_050; sg562_dive_051; sg562_dive_052; sg562_dive_053; sg562_dive_054; sg562_dive_055; sg562_dive_056; sg562_dive_057; sg562_dive_058; sg562_dive_059; sg562_dive_060; sg562_dive_061; sg562_dive_062; sg562_dive_063; sg562_dive_064; sg562_dive_065; sg562_dive_066; sg562_dive_067; sg562_dive_068; sg562_dive_069; sg562_dive_070; sg562_dive_071; sg562_dive_072; sg562_dive_073; sg562_dive_074; sg562_dive_075; sg562_dive_076; sg562_dive_077; sg562_dive_078; sg562_dive_079; sg562_dive_080; sg562_dive_081; sg562_dive_082; sg562_dive_083; sg562_dive_084; sg562_dive_085; sg562_dive_086; sg562_dive_087; sg562_dive_088; sg562_dive_089; sg562_dive_090; sg562_dive_091; sg562_dive_092; sg562_dive_093; sg562_dive_094; sg562_dive_095; sg562_dive_096; sg562_dive_097; sg562_dive_098; sg562_dive_099; sg562_dive_100; sg562_dive_101; sg562_dive_102; sg562_dive_103; sg562_dive_104; sg562_dive_105; sg562_dive_106; sg562_dive_107; sg562_dive_108; sg562_dive_109; sg562_dive_110; sg562_dive_111; sg562_dive_112; sg562_dive_113; sg562_dive_114; sg562_dive_115; sg562_dive_116; sg562_dive_117; sg562_dive_118; sg562_dive_119; sg562_dive_120; sg562_dive_121; sg562_dive_122; sg562_dive_123; sg562_dive_124; sg562_dive_125; sg562_dive_126; sg562_dive_127; sg562_dive_128; sg562_dive_129; sg562_dive_130; sg562_dive_131; sg562_dive_132; sg562_dive_133; sg562_dive_134; sg562_dive_135; sg562_dive_136; sg562_dive_137; sg562_dive_138; sg562_dive_139; sg562_dive_140; sg562_dive_141; sg562_dive_142; sg562_dive_143; sg562_dive_144; sg562_dive_145; sg562_dive_146; sg562_dive_147; sg562_dive_148; sg562_dive_149; sg562_dive_150; sg562_dive_151; sg562_dive_152; sg562_dive_153; sg562_dive_154; sg562_dive_155; sg562_dive_156; sg562_dive_157; sg562_dive_158; sg562_dive_159; sg562_dive_160; sg562_dive_161; sg562_dive_162; sg562_dive_163; sg562_dive_164; sg562_dive_165; sg562_dive_166; sg562_dive_167; sg562_dive_168; sg562_dive_169; sg562_dive_170; sg562_dive_171; sg562_dive_172; sg562_dive_173; sg562_dive_174; sg562_dive_175; sg562_dive_176; sg562_dive_177; sg562_dive_178; sg562_dive_179; sg562_dive_180; sg562_dive_181; sg562_dive_182; sg562_dive_183; sg562_dive_184; sg562_dive_185; sg562_dive_186; sg562_dive_187; sg562_dive_188; sg562_dive_189; sg562_dive_190; sg562_dive_191; sg562_dive_192; sg562_dive_193; sg562_dive_194; sg562_dive_195; sg562_dive_196; sg562_dive_197; sg562_dive_198; sg562_dive_199; sg562_dive_200; sg562_dive_201; sg562_dive_202; sg562_dive_203; sg562_dive_204; sg562_dive_205; sg562_dive_206; sg562_dive_207; sg562_dive_208; sg562_dive_209; sg562_dive_210; sg562_dive_211; sg562_dive_212; sg562_dive_213; sg562_dive_214; sg562_dive_215; sg562_dive_216; sg562_dive_217; sg562_dive_218; sg562_dive_219; sg562_dive_220; sg562_dive_221; sg562_dive_222; sg562_dive_223; sg562_dive_224; sg562_dive_225; sg562_dive_226; sg562_dive_227; sg562_dive_228; sg562_dive_229; sg562_dive_230; sg562_dive_231; sg562_dive_232; sg562_dive_233; sg562_dive_234; sg562_dive_235; sg562_dive_236; sg562_dive_237; sg562_dive_238; sg562_dive_239; sg562_dive_240; sg562_dive_241; sg562_dive_242; sg562_dive_243; sg562_dive_244; sg562_dive_245; sg562_dive_246; sg562_dive_247; sg562_dive_248; sg562_dive_249; sg562_dive_250; sg562_dive_251; sg562_dive_252; sg562_dive_253; sg562_dive_254; sg562_dive_255; sg562_dive_256; sg562_dive_257; sg562_dive_258; sg562_dive_259; sg562_dive_260; sg562_dive_261; sg562_dive_262; sg562_dive_263; sg562_dive_264; sg562_dive_265; sg562_dive_266; sg562_dive_267; sg562_dive_268; sg562_dive_269; sg562_dive_270; sg562_dive_271; sg562_dive_272; sg562_dive_273; sg562_dive_274; sg562_dive_275; sg562_dive_276; sg562_dive_277; sg562_dive_278; sg562_dive_279; sg562_dive_280; sg562_dive_281; sg562_dive_282; sg562_dive_283; sg562_dive_284; sg562_dive_285; sg562_dive_286; sg562_dive_287; sg562_dive_288; sg562_dive_289; sg562_dive_290; sg562_dive_291; sg562_dive_292; sg562_dive_293; sg562_dive_294; sg562_dive_295; sg562_dive_296; sg562_dive_297; sg562_dive_298; sg562_dive_299; sg562_dive_300; sg562_dive_301; sg562_dive_302; sg562_dive_303; sg562_dive_304; sg562_dive_305; sg562_dive_306; sg562_dive_307; sg562_dive_308; sg562_dive_309; sg562_dive_310; sg562_dive_311; sg562_dive_312; sg562_dive_313; sg562_dive_314; sg562_dive_315; sg562_dive_316; sg562_dive_317; sg562_dive_318; sg562_dive_319; sg562_dive_320; sg562_dive_321; sg562_dive_322; sg562_dive_323; sg562_dive_324; sg562_dive_325; sg562_dive_326; sg562_dive_327; sg562_dive_328; sg562_dive_329; sg562_dive_330; sg562_dive_331; sg562_dive_332; sg562_dive_333; sg562_dive_334; sg562_dive_335; sg562_dive_336; sg562_dive_337; sg562_dive_338; sg562_dive_339; sg562_dive_340; sg562_dive_341; sg562_dive_342; sg562_dive_343; sg562_dive_344; sg562_dive_345; sg562_dive_346; sg562_dive_347; sg562_dive_348; sg562_dive_349; sg562_dive_350; sg562_dive_351; sg562_dive_352; sg562_dive_353; sg562_dive_354; sg562_dive_355; sg562_dive_356; sg562_dive_357; sg562_dive_358; sg562_dive_359; sg562_dive_360; sg562_dive_361; sg562_dive_362; sg562_dive_363; sg562_dive_364; sg562_dive_365; sg562_dive_366; sg562_dive_367; sg562_dive_368; sg562_dive_369; sg562_dive_370; sg562_dive_371; sg562_dive_372; sg562_dive_373; sg562_dive_374; sg562_dive_375; sg562_dive_376; sg562_dive_377; sg562_dive_378; sg562_dive_379; sg562_dive_380; sg562_dive_381; sg562_dive_382; sg562_dive_383; sg562_dive_384; sg562_dive_385; sg562_dive_386; sg562_dive_387; sg562_dive_388; sg562_dive_389; sg562_dive_390; sg562_dive_391; sg562_dive_392; sg562_dive_393; sg562_dive_394; sg562_dive_395; sg562_dive_396; sg562_dive_397; sg562_dive_398; sg562_dive_399; sg562_dive_400; sg562_dive_401; sg562_dive_402; sg562_dive_403; sg562_dive_404; sg562_dive_405; sg562_dive_406; sg562_dive_407; sg562_dive_408; sg562_dive_409; sg562_dive_410; sg562_dive_411; sg562_dive_412; sg562_dive_413; sg562_dive_414; sg562_dive_415; sg562_dive_416; sg562_dive_417; sg562_dive_418; sg562_dive_419; sg562_dive_420; sg562_dive_421; sg562_dive_422; sg562_dive_423; sg562_dive_424; sg562_dive_425; sg562_dive_426; sg562_dive_427; sg562_dive_428; sg562_dive_429; sg562_dive_430; sg562_dive_431; sg562_dive_432; sg562_dive_433; sg562_dive_434; sg562_dive_435; sg562_dive_436; sg562_dive_437; sg562_dive_438; sg562_dive_439; sg562_dive_440; sg562_dive_441; sg562_dive_442; sg562_dive_443; sg562_dive_444; sg562_dive_445; sg562_dive_446; sg562_dive_447; sg562_dive_448; sg562_dive_449; sg562_dive_450; sg562_dive_451; sg562_dive_452; sg562_dive_453; sg562_dive_454; sg562_dive_455; sg562_dive_456; sg562_dive_457; sg562_dive_458; sg562_dive_459; sg562_dive_460; sg562_dive_461; sg562_dive_462; sg562_dive_463; sg562_dive_464; sg562_dive_465; sg562_dive_466; sg562_dive_467; sg562_dive_468; sg562_dive_469; sg562_dive_470; sg562_dive_471; sg562_dive_472; sg562_dive_473; sg562_dive_474; sg562_dive_475; sg562_dive_476; sg562_dive_477; sg562_dive_478; sg562_dive_479; sg562_dive_480; sg562_dive_481; sg562_dive_482; sg562_dive_483; sg562_dive_484; sg562_dive_485; sg562_dive_486; sg562_dive_487; sg562_dive_488; sg562_dive_489; sg562_dive_490; sg562_dive_491; sg562_dive_492;
    Type: Dataset
    Format: text/tab-separated-values, 1613333 data points
    Location Call Number Expected Availability
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  • 7
    Publication Date: 2024-02-26
    Keywords: DATE/TIME; DEPTH, water; Event label; GLD; Glider; LATITUDE; LONGITUDE; North Atlantic; Pressure, water; Salinity; sg559_dive_001; sg559_dive_002; sg559_dive_003; sg559_dive_004; sg559_dive_005; sg559_dive_006; sg559_dive_007; sg559_dive_008; sg559_dive_009; sg559_dive_010; sg559_dive_011; sg559_dive_012; sg559_dive_013; sg559_dive_014; sg559_dive_015; sg559_dive_016; sg559_dive_017; sg559_dive_018; sg559_dive_019; sg559_dive_020; sg559_dive_021; sg559_dive_022; sg559_dive_023; sg559_dive_024; sg559_dive_025; sg559_dive_026; sg559_dive_027; sg559_dive_028; sg559_dive_029; sg559_dive_030; sg559_dive_031; sg559_dive_032; sg559_dive_033; sg559_dive_034; sg559_dive_035; sg559_dive_036; sg559_dive_037; sg559_dive_038; sg559_dive_039; sg559_dive_040; sg559_dive_041; sg559_dive_042; sg559_dive_043; sg559_dive_044; sg559_dive_045; sg559_dive_046; sg559_dive_047; sg559_dive_048; sg559_dive_049; sg559_dive_050; sg559_dive_051; sg559_dive_052; sg559_dive_053; sg559_dive_054; sg559_dive_055; sg559_dive_056; sg559_dive_057; sg559_dive_058; sg559_dive_059; sg559_dive_060; sg559_dive_061; sg559_dive_062; sg559_dive_063; sg559_dive_064; sg559_dive_065; sg559_dive_066; sg559_dive_067; sg559_dive_068; sg559_dive_069; sg559_dive_070; sg559_dive_071; sg559_dive_072; sg559_dive_073; sg559_dive_074; sg559_dive_075; sg559_dive_076; sg559_dive_077; sg559_dive_078; sg559_dive_079; sg559_dive_080; sg559_dive_081; sg559_dive_082; sg559_dive_083; sg559_dive_084; sg559_dive_085; sg559_dive_086; sg559_dive_087; sg559_dive_088; sg559_dive_089; sg559_dive_090; sg559_dive_091; sg559_dive_092; sg559_dive_093; sg559_dive_094; sg559_dive_095; sg559_dive_096; sg559_dive_097; sg559_dive_098; sg559_dive_099; sg559_dive_100; sg559_dive_101; sg559_dive_102; sg559_dive_103; sg559_dive_104; sg559_dive_105; sg559_dive_106; sg559_dive_107; sg559_dive_108; sg559_dive_109; sg559_dive_110; sg559_dive_111; sg559_dive_112; sg559_dive_113; sg559_dive_114; sg559_dive_115; sg559_dive_116; sg559_dive_117; sg559_dive_118; sg559_dive_119; sg559_dive_120; sg559_dive_121; sg559_dive_122; sg559_dive_123; sg559_dive_124; sg559_dive_125; sg559_dive_126; sg559_dive_127; sg559_dive_128; sg559_dive_129; sg559_dive_130; sg559_dive_131; sg559_dive_132; sg559_dive_133; sg559_dive_134; sg559_dive_135; sg559_dive_136; sg559_dive_137; sg559_dive_138; sg559_dive_139; sg559_dive_140; sg559_dive_141; sg559_dive_142; sg559_dive_143; sg559_dive_144; sg559_dive_145; sg559_dive_146; sg559_dive_147; sg559_dive_148; sg559_dive_149; sg559_dive_150; sg559_dive_151; sg559_dive_152; sg559_dive_153; sg559_dive_154; sg559_dive_155; sg559_dive_156; sg559_dive_157; sg559_dive_158; sg559_dive_159; sg559_dive_160; sg559_dive_161; sg559_dive_162; sg559_dive_163; sg559_dive_164; sg559_dive_165; sg559_dive_166; sg559_dive_167; sg559_dive_168; sg559_dive_169; sg559_dive_170; sg559_dive_171; sg559_dive_172; sg559_dive_173; sg559_dive_174; sg559_dive_175; sg559_dive_176; sg559_dive_177; sg559_dive_180; sg559_dive_181; sg559_dive_182; sg559_dive_183; sg559_dive_184; sg559_dive_185; sg559_dive_186; sg559_dive_187; sg559_dive_188; sg559_dive_189; sg559_dive_190; sg559_dive_191; sg559_dive_192; sg559_dive_193; sg559_dive_194; sg559_dive_195; sg559_dive_196; sg559_dive_197; sg559_dive_198; sg559_dive_199; sg559_dive_200; sg559_dive_201; sg559_dive_202; sg559_dive_203; sg559_dive_204; sg559_dive_205; sg559_dive_206; sg559_dive_207; sg559_dive_208; sg559_dive_209; sg559_dive_210; sg559_dive_211; sg559_dive_212; sg559_dive_213; sg559_dive_214; sg559_dive_215; sg559_dive_216; sg559_dive_217; sg559_dive_218; sg559_dive_219; sg559_dive_220; sg559_dive_221; sg559_dive_222; sg559_dive_223; sg559_dive_224; sg559_dive_225; sg559_dive_226; sg559_dive_227; sg559_dive_228; sg559_dive_229; sg559_dive_230; sg559_dive_231; sg559_dive_232; sg559_dive_233; sg559_dive_234; sg559_dive_235; sg559_dive_236; sg559_dive_237; sg559_dive_238; sg559_dive_239; sg559_dive_240; sg559_dive_241; sg559_dive_242; sg559_dive_243; sg559_dive_244; sg559_dive_245; sg559_dive_246; 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    Type: Dataset
    Format: text/tab-separated-values, 1734596 data points
    Location Call Number Expected Availability
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  • 8
    Publication Date: 2024-02-26
    Keywords: DATE/TIME; DEPTH, water; Event label; GLD; Glider; LATITUDE; LONGITUDE; North Atlantic; Pressure, water; Salinity; sg564_dive_001; sg564_dive_002; sg564_dive_003; sg564_dive_004; sg564_dive_005; sg564_dive_006; sg564_dive_007; sg564_dive_008; sg564_dive_009; sg564_dive_010; sg564_dive_011; sg564_dive_012; sg564_dive_013; sg564_dive_014; sg564_dive_015; sg564_dive_016; sg564_dive_017; sg564_dive_018; sg564_dive_019; sg564_dive_020; sg564_dive_021; sg564_dive_022; sg564_dive_023; sg564_dive_024; sg564_dive_025; sg564_dive_026; sg564_dive_027; sg564_dive_028; sg564_dive_029; sg564_dive_030; sg564_dive_031; sg564_dive_032; sg564_dive_033; sg564_dive_034; sg564_dive_035; sg564_dive_036; sg564_dive_037; sg564_dive_038; sg564_dive_039; sg564_dive_040; sg564_dive_041; sg564_dive_042; sg564_dive_043; sg564_dive_044; sg564_dive_045; sg564_dive_046; sg564_dive_047; sg564_dive_048; sg564_dive_049; sg564_dive_050; sg564_dive_051; sg564_dive_052; sg564_dive_053; sg564_dive_054; sg564_dive_055; 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sg564_dive_434; sg564_dive_435; sg564_dive_436; sg564_dive_437; sg564_dive_438; sg564_dive_439; sg564_dive_440; sg564_dive_441; sg564_dive_442; sg564_dive_443; sg564_dive_444; sg564_dive_445; sg564_dive_446; sg564_dive_447; sg564_dive_448; sg564_dive_449; sg564_dive_450; sg564_dive_451; sg564_dive_452; sg564_dive_453; sg564_dive_454; sg564_dive_455; sg564_dive_456; sg564_dive_457; sg564_dive_458; sg564_dive_459; sg564_dive_460; sg564_dive_461; sg564_dive_462; sg564_dive_463; sg564_dive_464; sg564_dive_465; sg564_dive_466; sg564_dive_467; sg564_dive_468; sg564_dive_469; sg564_dive_470; sg564_dive_471; sg564_dive_472; sg564_dive_473; sg564_dive_474; sg564_dive_475; sg564_dive_476; sg564_dive_477; sg564_dive_478; sg564_dive_479; sg564_dive_480; sg564_dive_481; sg564_dive_482; sg564_dive_483; sg564_dive_484; sg564_dive_485; sg564_dive_486; sg564_dive_487; sg564_dive_488; sg564_dive_489; sg564_dive_490; sg564_dive_491; sg564_dive_492;
    Type: Dataset
    Format: text/tab-separated-values, 1840467 data points
    Location Call Number Expected Availability
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  • 9
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Våge, Kjetil; Papritz, Lukas; Håvik, Lisbeth; Spall, Michael; Moore, Kent (2018): Ocean convection linked to the recent ice edge retreat along east Greenland. Nature Communications, 9(1), https://doi.org/10.1038/s41467-018-03468-6
    Publication Date: 2024-02-26
    Description: Warm subtropical-origin Atlantic water flows northward across the Greenland-Scotland Ridge into the Nordic Seas, where it relinquishes heat to the atmosphere and gradually transforms into dense Atlantic-origin water. Returning southward along east Greenland, this water mass is situated beneath a layer of cold, fresh surface water and sea ice. Here we show, using measurements from autonomous ocean gliders, that the Atlantic-origin water was re-ventilated while transiting the western Iceland Sea during winter. This re-ventilation is a recent phenomenon made possible by the retreat of the ice edge toward Greenland. The fresh surface layer that characterises this region in summer is diverted onto the Greenland shelf by enhanced onshore Ekman transport induced by stronger northerly winds in fall and winter. Severe heat loss from the ocean offshore of the ice edge subsequently triggers convection, which further transforms the Atlantic-origin water. This re-ventilation is a counterintuitive occurrence in a warming climate, and highlights the difficulties inherent in predicting the behaviour of the complex coupled climate system.
    Type: Dataset
    Format: application/zip, 3 datasets
    Location Call Number Expected Availability
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  • 10
    Publication Date: 2022-05-25
    Description: © The Author(s), 2018. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Nature Communications 9 (2018): 1287, doi:10.1038/s41467-018-03468-6.
    Description: Warm subtropical-origin Atlantic water flows northward across the Greenland-Scotland Ridge into the Nordic Seas, where it relinquishes heat to the atmosphere and gradually transforms into dense Atlantic-origin water. Returning southward along east Greenland, this water mass is situated beneath a layer of cold, fresh surface water and sea ice. Here we show, using measurements from autonomous ocean gliders, that the Atlantic-origin water was re-ventilated while transiting the western Iceland Sea during winter. This re-ventilation is a recent phenomenon made possible by the retreat of the ice edge toward Greenland. The fresh surface layer that characterises this region in summer is diverted onto the Greenland shelf by enhanced onshore Ekman transport induced by stronger northerly winds in fall and winter. Severe heat loss from the ocean offshore of the ice edge subsequently triggers convection, which further transforms the Atlantic-origin water. This re-ventilation is a counterintuitive occurrence in a warming climate, and highlights the difficulties inherent in predicting the behaviour of the complex coupled climate system.
    Description: Support for this work was provided by the Norwegian Research Council under Grant agreement no. 231647 (L.H. and K.V.), the Bergen Research Foundation under Grant BFS2016REK01 (K.V.), and the Centre for Climate Dynamics at the Bjerknes Centre through the FRESHWATER project (K.V.). Additional funding was provided by the Swiss National Science Foundation grants P2EZP2162267 and P300P2174307 (L.P.), the National Science Foundation grant OCE-1558742 (M.A.S.), the Norway Fulbright Foundation (K.V.), the Canada Fulbright Foundation (G.W.K.M.), and the Natural Sciences and Engineering Research Council of Canada (G.W.K.M.).
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Location Call Number Expected Availability
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