From ebcc86561dabf3974ca11151445e66c0df4431f1 Mon Sep 17 00:00:00 2001 From: Bryan Newbold Date: Wed, 16 Dec 2020 14:33:52 -0800 Subject: improve release elasticsearch transform test coverage --- python/tests/files/release_3mssw2qnlnblbk7oqyv2dafgey.json | 1 + 1 file changed, 1 insertion(+) create mode 100644 python/tests/files/release_3mssw2qnlnblbk7oqyv2dafgey.json (limited to 'python/tests/files/release_3mssw2qnlnblbk7oqyv2dafgey.json') diff --git a/python/tests/files/release_3mssw2qnlnblbk7oqyv2dafgey.json b/python/tests/files/release_3mssw2qnlnblbk7oqyv2dafgey.json new file mode 100644 index 00000000..1c559509 --- /dev/null +++ b/python/tests/files/release_3mssw2qnlnblbk7oqyv2dafgey.json @@ -0,0 +1 @@ +{"abstracts":[{"sha1":"b2523f13fc2aa730a2e2336f27d448644074e24f","content":"

Jakobshavn Isbræ, West Greenland, which holds a 0.6-m sea level volume equivalent, has been speeding up and retreating since the late 1990s. Interpretation of its retreat has been hindered by difficulties in measuring its ice thickness with airborne radar depth sounders. Here, we employ high-resolution, helicopter-borne gravity data from 2012 to reconstruct its bed elevation within 50 km of the ocean margin using a three-dimensional inversion constrained by fjord bathymetry data offshore and a mass conservation algorithm inland. We find the glacier trough to be asymmetric and several 100 m deeper than estimated previously in the lower part. From 1996-2016, the grounding line migrated at 0.6 km/yr from 700 m to 1,100 m depth. Upstream, the bed drops to 1,600 m over 10 km then slowly climbs to 1,200 m depth in 40 km. Jakobshavn Isbræ will continue to retreat along a retrograde slope for decades to come.\n\nAn L., E. Rignot, S.H.P. Elieff, M. Morlighem, R. Millan, J. Mouginot, D.M. Holland, D. Holland, and J. Paden (2017), Bed elevation of Jakobshavn Isbræ, West Greenland, from high-resolution airborne gravity and other data, Geophys. Res. Lett., 44, doi:10.1002/2017GL073245.\n\n

","mimetype":"text/html"}],"refs":[],"contribs":[{"raw_name":"Lu An","role":"author","raw_affiliation":"University of California, Irvine"}],"license_slug":"CC-BY","publisher":"UC Irvine","ext_ids":{"doi":"10.7280/d1j37z"},"release_year":2018,"release_type":"dataset","webcaptures":[],"filesets":[{"release_ids":["3mssw2qnlnblbk7oqyv2dafgey"],"urls":[{"url":"https://merritt.cdlib.org/u/ark%3A%2F13030%2Fm5rg0r8q/1","rel":"repo-bundle"},{"url":"https://merritt.cdlib.org/d/ark%3A%2F13030%2Fm5rg0r8q/1/","rel":"repo"},{"url":"dat://77e94744aa5f967e6ed7e3990bfc29f141dbf2c0fff572eb1212b3bd706882f4/files/","rel":"dweb"}],"manifest":[{"path":"JKS_BedElevation_An_etal_2017.nc","size":736484,"md5":"af738fa325833a56bf947622958fd504","sha1":"443f1867b3a56132905e8d611ad03445d8134d3c","sha256":"52438ef0035b391027e989f00208de5c16ab8f9ff619aa7f45e998d6214a452f","extra":{"mimetype":"application/x-netcdf"}}],"state":"active","ident":"ho376wmdanckpp66iwfs7g22ne","revision":"e07ab7b0-bc0e-4da2-9121-542263e84e2d","extra":{"cdl_dash":{"version":1}}}],"files":[],"work_id":"pbf2dmuu5jf4dac2k22gxsjk6y","title":"Jakobshavn Glacier Bed Elevation","state":"active","ident":"3mssw2qnlnblbk7oqyv2dafgey","revision":"23040a75-2aa6-49f2-af3c-a5c12dcceffe","extra":{"ark_id":"ark:/13030/m5rg0r8q","cdl_dash":{"version":1}}} \ No newline at end of file -- cgit v1.2.3