{"doi":"10.1007/s12665-015-4301-2","title":"Fluctuation of glaciers in the southeast Russian Altai and northwest Mongolia Mountains since the Little Ice Age maximum","abstract":null,"journal":"Environmental Earth Sciences","year":2015,"id":34489,"datarank":2.2243866625357995,"base_score":3.6635616461296463,"endowment":3.6635616461296463,"self_citation_contribution":0.5495342469194471,"citation_network_contribution":1.6748524156163522,"self_endowment_contribution":0.5495342469194471,"citer_contribution":1.6748524156163522,"corpus_percentile":null,"corpus_rank":null,"citation_count":38,"citer_count":29,"citers_with_citation_signal":28,"citers_with_endowment":28,"datacite_reuse_total":0,"is_dataset":false,"is_dataset_confidence":null,"is_data_producer":false,"deposit_databanks":null,"is_oa":false,"file_count":0,"downloads":0,"has_version_chain":false,"published_date":null,"fair_score":null,"fair_percentile":null,"algorithm_id":"datarank_citation_only_1hop_v6","ranking_scope":"data_only","authors":[{"id":178579,"name":"Kirill Chistyakov","orcid":null,"position":1,"is_corresponding":false},{"id":178580,"name":"Elena Kunaeva","orcid":null,"position":2,"is_corresponding":false},{"id":178577,"name":"Dmitry Ganiushkin","orcid":null,"position":0,"is_corresponding":false}],"reference_count":0,"raw_metadata":{"has_enrichment":true,"base_score":3.6635616461296463,"endowment":3.6635616461296463,"datacite_reuse_total":0,"file_count":0,"downloads":0,"views":0,"has_version_chain":false,"is_dataset":false,"is_oa":false,"pmid":"24523987","pmcid":null,"openalex_id":"https://openalex.org/W2039728448","authors":[],"funders":[],"total_grants":0,"fwci":4.5041,"citation_percentile":0.94383157,"influential_citations":0,"citation_trend":[{"year":2015,"count":10},{"year":2016,"count":2},{"year":2017,"count":5},{"year":2018,"count":3},{"year":2019,"count":2},{"year":2020,"count":3},{"year":2021,"count":3},{"year":2022,"count":6},{"year":2023,"count":3},{"year":2025,"count":1}],"oa_status":"closed","license":"http://www.springer.com/tdm","oa_locations":[{"url":"http://link.springer.com/content/pdf/10.1007/s12665-015-4301-2.pdf","host_type":"publisher"},{"url":"http://link.springer.com/article/10.1007/s12665-015-4301-2/fulltext.html","host_type":"publisher"},{"url":"http://link.springer.com/content/pdf/10.1007/s12665-015-4301-2","host_type":"publisher"},{"url":"https://doi.org/10.1007/s12665-015-4301-2","host_type":"journal"}],"fields_of_study":["Geology and Paleoclimatology Research","Cryospheric studies and observations","Climate change and permafrost","Geology","Environmental Science","Geography"],"mesh_terms":[],"keywords":["Glacier","Glacial period","Geology","Physical geography","Firn","Snow","Ice field","Accumulation zone","Glacier morphology","Snow line","Climatology","Geomorphology","Geography","Cryosphere","Ice stream","Snow cover","Sea ice"],"sdg_mappings":[],"linked_datasets":[],"clinical_trials":[],"software_tools":[],"database_accessions":[],"source":"live","citation_network_status":"fetched"},"created_at":"2026-06-09T18:50:04.427215Z","pmid":null,"pmcid":null,"fwci":null,"citation_percentile":null,"influential_citations":0,"oa_status":null,"license":null,"views":0,"total_file_size_bytes":0,"version_count":0,"fair_f":null,"fair_a":null,"fair_i":null,"fair_r":null,"fair_zscore":null,"fair_rationale":null,"fair_model":null,"fair_agent_version":null,"fair_fulltext_source":null,"fair_has_llm":null,"fair_computed_at":null,"clinical_trials":[],"software_tools":[],"db_accessions":[],"linked_datasets":[],"topics":[]}