diff --git a/README.md b/README.md index 2ff88fd..3e5b708 100644 --- a/README.md +++ b/README.md @@ -12,7 +12,7 @@ `WOS_API_KEY` dans mon mail CNRS. -- [ ] concaténer titre et abstract pour teeft +- [x] concaténer titre et abstract pour teeft - [ ] ajouter les reprint_addresses (affiliations) - [ ] enrichissement service web base Pascal (?) diff --git a/data/corpus-simple-teeft-en-50.json b/data/corpus-simple-teeft-en-50.json index 6a38bcf..deb5cd3 100644 --- a/data/corpus-simple-teeft-en-50.json +++ b/data/corpus-simple-teeft-en-50.json @@ -94,11 +94,11 @@ "eastern tropical pacific", "amo", "phase transition", + "climate impacts", "eastern tropical pacific sea surface temperature sst", "wide variety", "data sets", - "results show", - "diagnostic analysis" + "results show" ] } }, @@ -151,13 +151,13 @@ "c-ant", "oceanic", "pgc", + "anthropogenic", "ocean circulation", "pgc yr", + "oceanic anthropogenic co", "industrial era", "oceanic c-ant", - "new estimate", - "oceanic anthropogenic co", - "potential temperature salinity radiocarbon" + "new estimate" ] } }, @@ -447,16 +447,16 @@ "rnsr_id": [], "instituts": [], "teeft": [ + "antarctica's", "vertical levels", + "antarctica's surface winds", "southern ocean", "antarctica's katabatic winds", "strongest near-surface winds", "consistent ones", "strong surface", "atmospheric component", - "global climate model ec-earth", - "sea surface temperature sst simulations", - "present day" + "global climate model ec-earth" ] } }, @@ -496,7 +496,18 @@ "etab": [], "rnsr_id": [], "instituts": [], - "teeft": "One of the key components of Antarctica's harsh climate is its renowned katabatic winds, which are among the fiercest surface winds on Earth. Caused primarily by strong surface cooling over the sloping ice surface, these semipermanent winds result primarily from the strong surface temperature inversion and associated temperature deficit between the surface layer and the free atmosphere aloft. Katabatic winds exert a strong effect on the mass budget of the Antarctic ice sheet by affecting snowdrift (sublimation) and by (partially) regulating the net atmospheric moisture transports toward the Antarctic. It has been suggested that greenhouse warming may lead to reduced surface cooling and weakened katabatic winds. This is tested by using a global climate model (EC-Earth) in prescribed sea surface temperature simulations of the present-day (2002-2006) and future (2094-2098) climates. Because simulated topographically induced katabatic winds are likely to depend on the model grid, we employ two model resolutions: (1) T159L62 (similar to 100 km, 62 vertical levels) and (2) T799L91 (similar to 20 km, 91 vertical levels). It is shown here that present-day surface winds over Antarctica in high resolution are generally stronger than in low resolution, especially in the escarpment region with its steep orography. Simulated surface winds are generally underestimated with respect to observations, in particular the strongest winds (occurring over steep slopes), and especially in low resolution. The seasonal cycle in surface winds is simulated fairly accurately. Surface temperatures are also relatively well simulated (when corrected for elevation differences), especially in high resolution." + "teeft": [ + "katabatic", + "katabatic winds", + "vertical levels", + "high resolution", + "low resolution", + "surface winds", + "key components", + "antarctica's harsh climate", + "renowned katabatic winds", + "fiercest surface winds" + ] } }, { @@ -625,7 +636,7 @@ "monoterpene", "sesquiterpene", "lpj-guess", - "millennial variability" + "terrestrial vegetation" ] } }, @@ -673,14 +684,14 @@ "teeft": [ "china's", "precipitation", - "nh", - "china's precipitation", "volcanic aerosols", + "china's precipitation", "china's monsoon precipitation", "monsoon asia drought atlas", "both reconstructions four categories", "northern hemisphere nh injection", - "epoch analysis sea" + "epoch analysis sea", + "monte carlo" ] } }, @@ -725,13 +736,13 @@ "climate models", "simulations", "cloud temperature", + "low-cloud optical depth feedback", "low-level cloud optical depth", "surface air temperature", "control climate", "cloud optical depth-temperature relationships", "climate model behavior", - "control climate simulations", - "optical depth feedback" + "control climate simulations" ] } }, @@ -778,6 +789,7 @@ "rnsr_id": [], "instituts": [], "teeft": [ + "high elevations", "global solar irradiance", "high-elevation sites", "maui hawai i", @@ -786,8 +798,7 @@ "linear regression analysis", "dry season may-october", "significant p", - "positive trends", - "four high-elevation stations" + "positive trends" ] } }, @@ -938,13 +949,13 @@ "stratospheric", "slp", "tropospheric", + "cmip", "stratospheric wind change", "intermodel spread", "slp change", "stratosphere", "future changes", - "stratospheric circulation", - "important impact" + "stratospheric circulation" ] } }, @@ -995,13 +1006,13 @@ "rcp", "poleward", "ozone recovery", - "antarctic", "depletion period", "summer poleward shift", "ozone", "century antarctic ozone depletion", "greenhouse gases ghgs", - "conspicuous atmospheric circulation trends" + "conspicuous atmospheric circulation trends", + "southern hemisphere sh" ] } }, @@ -1052,15 +1063,15 @@ "instituts": [], "teeft": [ "fast-ice", - "breakout", "sea-ice", + "breakout", + "weddell", + "northern weddell sea", "winter fast-ice", "orkney islands northern weddell sea antarctica", "century long", "longest observational record", - "sea-ice variability", - "southern hemisphere", - "present analyses" + "sea-ice variability" ] } }, @@ -1093,7 +1104,12 @@ "etab": [], "rnsr_id": [], "instituts": [], - "teeft": "" + "teeft": [ + "global model projections", + "climate change", + "case study", + "wrf models" + ] } }, { @@ -1142,7 +1158,10 @@ "etab": [], "rnsr_id": [], "instituts": [], - "teeft": "" + "teeft": [ + "climatic effects", + "cirrus clouds" + ] } }, { @@ -1188,7 +1207,12 @@ "etab": [], "rnsr_id": [], "instituts": [], - "teeft": "" + "teeft": [ + "postlaunch calibration", + "bias characterization", + "amsu-a upper air", + "gps ro" + ] } }, { @@ -1295,15 +1319,15 @@ "instituts": [], "teeft": [ "tropospheric", - "ppbv", "ppbv k", "eastern pacific", - "stratospheric", "horizontal resolution", "ozone changes", "tropospheric ozone", "midlatitude lower stratosphere", - "tropospheric chemistry" + "tropospheric chemistry", + "global burden", + "ozone" ] } }, @@ -1346,12 +1370,12 @@ "surface temperature trends", "aerosol concentration", "aerosol indirect effects", + "sophisticated parameterizations", "temperature trend bias", "more regions", "clear difference", "model output", - "model intercomparison project phase", - "latitudinal distribution" + "model intercomparison project phase" ] } }, @@ -1529,13 +1553,13 @@ "lig", "insolation", "western african precipitation", + "western african rainfall", "study documents", "long-term evolution", "last interglacial lig", "geochemical records", "nine sediment cores", - "western african margin", - "transient simulation" + "western african margin" ] } }, @@ -1654,6 +1678,7 @@ "instituts": [], "teeft": [ "qbo", + "teleconnection", "predictability", "quasi-biennial oscillation qbo", "climate forecasts", @@ -1661,8 +1686,7 @@ "ocean-atmosphere climate models", "internal atmospheric processes", "correlation scores", - "observational analyses", - "lead time" + "observational analyses" ] } }, @@ -1711,14 +1735,14 @@ "teeft": [ "qbo", "stratospheric", + "quasi-biennial", "sulfur dioxide", "tg yr", + "quasi-biennial oscillation", "stratospheric sulfate aerosol", "quasi-biennial oscillation qbo", "nasa goddard earth", - "system version", - "chemistry climate model", - "year simulations" + "system version" ] } }, @@ -1759,6 +1783,7 @@ "rnsr_id": [], "instituts": [], "teeft": [ + "meridional", "net radiation", "feedback", "model intercomparison project phase", @@ -1767,8 +1792,7 @@ "meridional energy transport", "greenhouse gas longwave", "low latitudes", - "equator-to-pole net radiation gradient", - "poleward energy transport" + "equator-to-pole net radiation gradient" ] } }, @@ -1816,10 +1840,10 @@ "instituts": [], "teeft": [ "idw", - "large-scale events", "interpolation", - "rainfall data", "interpolation techniques", + "large-scale events", + "rainfall data", "high station density", "high-resolution gridded", "data sets", @@ -1889,12 +1913,12 @@ "sulfate", "side effects", "sulfate aerosols", + "model intercomparison project", "polar regions", "uv-b radiation", "ozone", "stratospheric sulfate aerosols", - "anthropogenic co", - "stratospheric injections" + "anthropogenic co" ] } }, @@ -1944,13 +1968,13 @@ "cirrus", "nucleation", "cirrus clouds", + "ice nuclei", "upper troposphere", "effect cirrus clouds", "crucial role", "climate system", "mechanism cem", - "high cloud", - "efficient ice nuclei" + "high cloud" ] } }, @@ -2009,15 +2033,15 @@ "instituts": [], "teeft": [ "sstas", + "interannual", "interannual variation", + "wet season onsets", "wet season onset", "southern amazon", - "wet season onsets", + "total variance", "amazon", "previous studies", - "sea surface temperature anomalies sstas", - "tropical pacific", - "causes such" + "sea surface temperature anomalies sstas" ] } }, @@ -2289,14 +2313,14 @@ "teeft": [ "climate sensitivity", "poleward", + "dynamical sensitivity", + "southern hemisphere", "poleward expansion", "hadley circulation", "subtropical dry zone", "midlatitude jet", - "model intercomparison project phase", - "southern hemisphere dynamical response", - "greenhouse gas", - "three metrics" + "dynamical", + "model intercomparison project phase" ] } }, @@ -2345,15 +2369,15 @@ "instituts": [], "teeft": [ "ohu", + "feedbacks", + "spatial pattern", "ocean heat uptake ohu", "transient global", "multimodel framework", "simple heat", "shallow aquaplanet ocean", "atmospheric general circulation models", - "high latitudes", - "distinct modes", - "tropical ohu" + "high latitudes" ] } }, @@ -2394,14 +2418,14 @@ "teeft": [ "stratospheric", "climate sensitivity", + "negative feedback", "stratospheric water vapor", "feedback", "climate chemistry models ccms", "feedback mechanisms", "climate change simulations", "chemical feedback", - "radiative feedback", - "ozone changes" + "radiative feedback" ] } }, @@ -2534,12 +2558,12 @@ "INSU" ], "teeft": [ + "optimal fingerprinting", + "multiple sources", "inference procedure", "attribution studies", "use linear regression methods", - "optimal fingerprinting", "latter methodological paradigm", - "multiple sources", "climate responses", "instance internal variability climate model error", "observational error", @@ -2658,9 +2682,9 @@ "long-term sensitivity", "tropical land carbon storage", "atmospheric co", + "emergent constraints", "emergent linear relationship", - "atmospheric carbon dioxide co", - "interannual temperature variability iav" + "atmospheric carbon dioxide co" ] } }, @@ -2727,7 +2751,10 @@ "etab": [], "rnsr_id": [], "instituts": [], - "teeft": "" + "teeft": [ + "multimodel examination", + "climate extremes" + ] } }, { @@ -2774,7 +2801,14 @@ "etab": [], "rnsr_id": [], "instituts": [], - "teeft": "" + "teeft": [ + "emissions", + "ammonia emissions", + "states european union", + "high-resolution inversion", + "ammonium wet deposition data interpretation", + "new agricultural emissions inventory" + ] } }, { @@ -2878,8 +2912,8 @@ "instituts": [], "teeft": [ "emissions", - "sghg", "radiative", + "sghg", "hfc", "atmospheric measurements show", "hydrofluorocarbons hfcs", diff --git a/enrich-teeft-en.ini b/enrich-teeft-en.ini index 2665481..4a79698 100644 --- a/enrich-teeft-en.ini +++ b/enrich-teeft-en.ini @@ -25,8 +25,7 @@ [assign] path = ws.teeft -# certains abstracts sont des tableaux, d'autres une chaîne. On veut envoyer une chaîne. -value = get("abstract", "") +value = fix(_.get(self, "abstract", ""), _.get(self, "title")).join(" ; ") [expand] path = ws.teeft