{"id":617,"date":"2021-07-17T10:46:23","date_gmt":"2021-07-17T09:46:23","guid":{"rendered":"https:\/\/www.iamas.org\/iccp\/?page_id=617"},"modified":"2021-07-19T11:34:04","modified_gmt":"2021-07-19T10:34:04","slug":"session-4-mixed-phase-clouds","status":"publish","type":"page","link":"https:\/\/www.iamas.org\/iccp\/session-4-mixed-phase-clouds\/","title":{"rendered":"Session 4 &#8211; Mixed phase clouds"},"content":{"rendered":"\n<p><strong>Oral session:<\/strong><\/p>\n\n\n\n<figure class=\"wp-block-table is-style-stripes\"><table><tbody><tr><td>S4.1 Microphysical cloud properties and cloud probes&#8217; benchmark during the Pallas Cloud Experiments (PaCE).<br>Konstantinos Doulgeris*<sup>1<\/sup>, Ari Leskinen<sup>2<\/sup>, Mika Komppula<sup>2<\/sup>, David Brus<sup>1<\/sup><br><em><sup>1<\/sup>Finnish Meteorological Institute, Finland, <sup>2<\/sup>Finnish Meteorological Institute, Finland<\/em> <a href=\"https:\/\/www.iamas.org\/iccp\/wp-content\/uploads\/sites\/3\/2021\/07\/session4_part1a.mp4\" target=\"_blank\" rel=\"noreferrer noopener\">(video; position 0:00)<\/a><\/td><\/tr><tr><td>S4.2 Liquid water content and effective radius retrievals in mixed-phase cloud layers from Cloud radar data based on the forward modeling<br>Yujun Qiu*<sup>1<\/sup>, Tom Choularton<sup>2<\/sup>, Jonny Crosier<sup>2<\/sup><br><em><sup>1<\/sup>Key Laboratory for Aerosol-Cloud-Precipitation of China Meteorological Administration, Nanjing University of Information Science &amp; Technology, China, <sup>2<\/sup>Centre for Atmospheric Science, SEAES,University of Manchester, UK<\/em> <a href=\"https:\/\/www.iamas.org\/iccp\/wp-content\/uploads\/sites\/3\/2021\/07\/session4_part1a.mp4\" data-type=\"URL\" data-id=\"https:\/\/www.iamas.org\/iccp\/wp-content\/uploads\/sites\/3\/2021\/07\/session4_part1a.mp4\" target=\"_blank\" rel=\"noreferrer noopener\">(video; position 15:35)<\/a><\/td><\/tr><tr><td>S4.3 Aircraft Observations of Liquid and Ice in Midlatitude Mixed-Phase Clouds<br>Zhen Zhao*, Heng-chi Lei<br><em>Institute of Atmospheric Physics,Chinese Academy of Sciences, China<\/em> <a href=\"https:\/\/www.iamas.org\/iccp\/wp-content\/uploads\/sites\/3\/2021\/07\/session4_part1a.mp4\" data-type=\"URL\" data-id=\"https:\/\/www.iamas.org\/iccp\/wp-content\/uploads\/sites\/3\/2021\/07\/session4_part1a.mp4\" target=\"_blank\" rel=\"noreferrer noopener\">(video; position 30:00)<\/a><\/td><\/tr><tr><td>S4.4 Vertical profiles of cloud properties measured with a holographic imager on a cable car<br>Alexander Beck*, Jan Henneberger, Zamin A. Kanji, Ulrike Lohmann<br><em>Institute of Atmospheric and Climate Science, ETH Zurich, Switzerland<\/em> <a href=\"https:\/\/www.iamas.org\/iccp\/wp-content\/uploads\/sites\/3\/2021\/07\/session4_part1b.mp4\" data-type=\"URL\" data-id=\"https:\/\/www.iamas.org\/iccp\/wp-content\/uploads\/sites\/3\/2021\/07\/session4_part1b.mp4\" target=\"_blank\" rel=\"noreferrer noopener\">(video; position 0:00)<\/a><\/td><\/tr><tr><td>S4.5 A detailed examination of the microphysical processes leading to ice production within an orographic wintertime cloud with freezing drizzle<br>Jeffrey French*<sup>1<\/sup>, Sarah Tessendorf<sup>2<\/sup>, Darcy Jacobson<sup>1<\/sup>, Roy Rasmussen<sup>2<\/sup>, Bart Geerts<sup>1<\/sup>, Binod Pokharel<sup>1<\/sup>, Lulin Xue<sup>1<\/sup>, Pat Holbrook<sup>3<\/sup>, Mel Kunkel<sup>3<\/sup>, Derek Blestrud<sup>3<\/sup>, Shaun Parkinson<sup>3<\/sup><br><em><sup>1<\/sup>University of Wyoming, USA, <sup>2<\/sup>NCAR\/RAL, USA, <sup>3<\/sup>Idaho Power Company, USA<\/em> <a href=\"https:\/\/www.iamas.org\/iccp\/wp-content\/uploads\/sites\/3\/2021\/07\/session4_part1b.mp4\" data-type=\"URL\" data-id=\"https:\/\/www.iamas.org\/iccp\/wp-content\/uploads\/sites\/3\/2021\/07\/session4_part1b.mp4\" target=\"_blank\" rel=\"noreferrer noopener\">(video; position 15:12)<\/a><\/td><\/tr><tr><td>S4.6 In-situ airborne observations of small ice in turbulent mixed phase altocumulus clouds.<br>Paul Barrett*<sup>1,2<\/sup>, Alan Blyth<sup>2,3<\/sup>, Philip R. A. Brown<sup>1<\/sup>, Zbigniew Ulanowski<sup>4<\/sup><br><em><sup>1<\/sup>Met Office, UK, <sup>2<\/sup>University of Leeds School of Earth and Environment, Institute for Climate and Atmospheric Science, UK, <sup>3<\/sup>National Centre for Atmospheric Science, University of Leeds, UK, <sup>4<\/sup>Centre for Atmospheric and Instrumentation Research, University of Hertfordshire, UK<\/em><a href=\"https:\/\/www.iamas.org\/iccp\/wp-content\/uploads\/sites\/3\/2021\/07\/session4_part1b.mp4\" data-type=\"URL\" data-id=\"https:\/\/www.iamas.org\/iccp\/wp-content\/uploads\/sites\/3\/2021\/07\/session4_part1b.mp4\" target=\"_blank\" rel=\"noreferrer noopener\"> (video; position 31:22)<\/a><\/td><\/tr><\/tbody><\/table><\/figure>\n\n\n\n<figure class=\"wp-block-table is-style-stripes\"><table><tbody><tr><td>S4.7 In situ and radar Doppler spectrum constraints of ice sticking efficiency and ice properties in a mid-latitude squall line<br>Marcus van Lier-Walqui*<sup>1,2<\/sup>, Ann Fridlind<sup>2<\/sup>, Andrew Ackerman<sup>2<\/sup>, Christopher Williams<sup>3<\/sup>, Greg McFarquhar<sup>4<\/sup>, Wei Wu<sup>4<\/sup>, Xiaowen Li<sup>5,6<\/sup>, Wei-Kuo Tao<sup>6<\/sup>, Alexei Korolev<sup>7<\/sup><br><em><sup>1<\/sup>Columbia University, USA, <sup>2<\/sup>NASA Goddard Institute For Space Studies, USA, <sup>3<\/sup>University of Colorado, USA, <sup>4<\/sup>University of Illinois, USA, <sup>5<\/sup>Morgan State University, USA, <sup>6<\/sup>NASA Goddard Space Flight Center, USA, <sup>7<\/sup>Environment Canada, Canada<\/em> <a href=\"https:\/\/www.iamas.org\/iccp\/wp-content\/uploads\/sites\/3\/2021\/07\/session4_part1c.mp4\" data-type=\"URL\" data-id=\"https:\/\/www.iamas.org\/iccp\/wp-content\/uploads\/sites\/3\/2021\/07\/session4_part1c.mp4\" target=\"_blank\" rel=\"noreferrer noopener\">(video; position 0:00)<\/a><\/td><\/tr><tr><td>S4.8 LIMA: A two-moment microphysical scheme driven by a multimodal population of cloud condensation and ice freezing nuclei<br>Jean-Pierre Pinty*<sup>1<\/sup>, Beno\u00eet Vi\u00e9<sup>2<\/sup>, Sarah Berthet<sup>3<\/sup>, Maud Leriche<sup>1<\/sup><br><em><sup>1<\/sup>Laboratoire d&#8217;A\u00e9rologie, UMR5560, CNRS\/Universit\u00e9 de Toulouse, France, <sup>2<\/sup>M\u00e9t\u00e9o-France, UMR3589, CNRS\/M\u00e9t\u00e9o-France, France, <sup>3<\/sup>LEGOS, UMR5566, CNES\/CNRS\/IRD\/Universit\u00e9 de Toulouse, France<\/em><br><a href=\"https:\/\/www.iamas.org\/iccp\/wp-content\/uploads\/sites\/3\/2021\/07\/session4_part1c.mp4\" data-type=\"URL\" data-id=\"https:\/\/www.iamas.org\/iccp\/wp-content\/uploads\/sites\/3\/2021\/07\/session4_part1c.mp4\" target=\"_blank\" rel=\"noreferrer noopener\">(video; position 15:00)<\/a><\/td><\/tr><tr><td>S4.9 Microphysics parameterization of explicit partial melting of snow to study the formation of freezing rain and ice pellets<br>M\u00e9lissa Cholette*, Julie M. Th\u00e9riault<br><em>University of Quebec at Montreal, Canada<\/em> <a href=\"https:\/\/www.iamas.org\/iccp\/wp-content\/uploads\/sites\/3\/2021\/07\/session4_part1c.mp4\" data-type=\"URL\" data-id=\"https:\/\/www.iamas.org\/iccp\/wp-content\/uploads\/sites\/3\/2021\/07\/session4_part1c.mp4\" target=\"_blank\" rel=\"noreferrer noopener\">(video; position 31:00)<\/a><\/td><\/tr><tr><td>S4.10 Effect of Evaporation on Midlatitude Continental Convective Clouds Experiment (MC3E) Melting Layer Simulations<br>Andrea Neumann*<sup>1<\/sup>, Michael Poellot<sup>1<\/sup>, Andrew Heymsfield<sup>2<\/sup>, Aaron Bansemer<sup>2<\/sup><br><em><sup>1<\/sup>University of North Dakota, USA, <sup>2<\/sup>National Center for Atmospheric Research, USA<\/em> <a href=\"https:\/\/www.iamas.org\/iccp\/wp-content\/uploads\/sites\/3\/2021\/07\/session4_part1d.mp4\" data-type=\"URL\" data-id=\"https:\/\/www.iamas.org\/iccp\/wp-content\/uploads\/sites\/3\/2021\/07\/session4_part1d.mp4\" target=\"_blank\" rel=\"noreferrer noopener\">(video; position 0:00)<\/a><\/td><\/tr><tr><td>S.4.11 Synthesis of observations and models using a new Bayesian framework for microphysical parameterization<br>Hugh Morrison<sup>1<\/sup>, Marcus van Lier-Walqui*<sup>2<\/sup>, Matthew Kumjian<sup>3<\/sup>, Olivier Prat<sup>4<\/sup><br><em><sup>1<\/sup>NCAR, USA, <sup>2<\/sup>Columbia University, USA, <sup>3<\/sup>Pennsylvania State University, USA, <sup>4<\/sup>North Carolina State University, USA<\/em> <a href=\"https:\/\/www.iamas.org\/iccp\/wp-content\/uploads\/sites\/3\/2021\/07\/session4_part1d.mp4\" data-type=\"URL\" data-id=\"https:\/\/www.iamas.org\/iccp\/wp-content\/uploads\/sites\/3\/2021\/07\/session4_part1d.mp4\" target=\"_blank\" rel=\"noreferrer noopener\">(video; position 15:00)<\/a><\/td><\/tr><tr><td>S4.12 Relationship between atmospheric aerosols, hail and polarimetric radar signatures in a mid-latitude storm<br>Eyal Ilotoviz<sup>1<\/sup>, Alexander Khain*<sup>1<\/sup>, Vaughan Phillips<sup>2<\/sup>, Alexander Ryzhkov<sup>3<\/sup><br><em><sup>1<\/sup>The Hebrew University of Jerusalem, Israel, <sup>2<\/sup>Lund University, Sweden, <sup>3<\/sup>University of Oklahoma, USA<\/em><br><a href=\"https:\/\/www.iamas.org\/iccp\/wp-content\/uploads\/sites\/3\/2021\/07\/session4_part1d.mp4\" data-type=\"URL\" data-id=\"https:\/\/www.iamas.org\/iccp\/wp-content\/uploads\/sites\/3\/2021\/07\/session4_part1d.mp4\" target=\"_blank\" rel=\"noreferrer noopener\">(video; position 30:31)<\/a><\/td><\/tr><\/tbody><\/table><\/figure>\n\n\n\n<p><strong>Poster session:<\/strong><\/p>\n\n\n\n<figure class=\"wp-block-table is-style-stripes\"><table><tbody><tr><td>P4.1 Analysis on the microphysical features of raindrop size distribution under different synoptic systems in mountainous area Fujian<br>Lin Wen*<sup>1<\/sup>, Lin Changcheng<sup>1<\/sup>, Yao Zhanyu<sup>2<\/sup>, Chen Binbin<sup>1<\/sup>, Li Dan<sup>1<\/sup>, Zheng Wenjun<sup>3<\/sup><br><em><sup>1<\/sup><\/em><em>Fujian Meteorological Science Institute, China, <sup>2<\/sup>Chinese Academy of Meteorological Science, China, <sup>3<\/sup>Youxi Meteorological Bureau, China<\/em><\/td><\/tr><tr><td>P4.2 Investigation of Riming within Mixed-phase Stratiform Clouds Using Weather Research and Forecasting (WRF) Model<br>Tuanjie Hou*, Hengchi Lei, Zhaoxia Hu<br><em>Institute of Atmospheric Physics, Chinese Academy of Sciences, China<\/em><\/td><\/tr><tr><td>P4.3 Investigation of Mass-Dimension Relationship Parameters Within a Surface of Equally Realizable Solutions<br>Joseph Finlon*<sup>1,3<\/sup>, Greg McFarquhar<sup>1,3<\/sup>, Robert Rauber<sup>1<\/sup>, Brian Jewett<sup>1<\/sup>, David Plummer<sup>1,2<\/sup>, Roy Rasmussen<sup>3<\/sup><br><em><sup>1<\/sup><\/em><em>University of Illinois at Urbana-Champaign, USA, <sup>2<\/sup>University of Wyoming, USA, <sup>3<\/sup>National Center for Atmospheric Research, USA<\/em><\/td><\/tr><tr><td>P4.4 Diffusion processes in mixed-phase clouds involving direct particle interactions<br>Manuel Baumgartner*, Peter Spichtinger<br><em>Johannes Gutenberg University, Germany<\/em><\/td><\/tr><tr><td>P4.5 Aerosol-cloud interactions over the Arctic using the Canadian atmospheric chemistry model GEM-MACH<br>Ana Cirisan*<sup>1<\/sup>, Sylvie Gravel<sup>2<\/sup>, Wanmin Gong<sup>3<\/sup>, Vickie Irish<sup>4<\/sup>, Allan Bertram<sup>4<\/sup>, \u00c9ric Girard<sup>1<\/sup><br><em><sup>1<\/sup><\/em><em>Universit\u00e9 du Qu\u00e9bec \u00e0 Montr\u00e9al, Canada, <sup>2<\/sup>Canadian Meteorological Centre, Canada, <sup>3<\/sup>Environment Canada, Canada, <sup>4<\/sup>Department of Chemistry, The University of British Columbia, Canada<\/em><\/td><\/tr><tr><td>P4.6 Modeling the melting of graupel and hail in a bulk microphysics parameterization<br>Axel Seifert*<sup>1<\/sup>, Vivek Sant<sup>2<\/sup><br><em><sup>1<\/sup><\/em><em>Deutscher Wetterdienst, Germany, <sup>2<\/sup>Max Planck Institute for Meteorology, Germany<\/em><\/td><\/tr><tr><td>P4.7 Implementing ice microphysics to a large eddy simulation model coupled with sectional aerosol module<br>Jaakko Ahola*<sup>1,3<\/sup>, Tomi Raatikainen<sup>1<\/sup>, Juha Tonttila<sup>2<\/sup>, Sami Romakkaniemi<sup>2<\/sup>, Hannele Korhonen<sup>1<\/sup><br><em><sup>1<\/sup><\/em><em>Finnish Meteorological Institute, Finland, <sup>2<\/sup>Finnish Meteorological Institute, Finland, <sup>3<\/sup>University of Turku, Finland<\/em><\/td><\/tr><tr><td>P4.8 Model simulations with COSMO-SPECS: Application of prognostic INP description for stratiform clouds<br>Martin Simmel*<sup>1<\/sup>, Matthias Lieber<sup>2<\/sup>, Oswald Knoth<sup>1<\/sup>, Ina Tegen<sup>1<\/sup><br><em><sup>1<\/sup><\/em><em>TROPOS Leibniz Institute for Tropospheric Research, Germany, <sup>2<\/sup>Center for Information Services and High Performance Computing (ZIH), TU Dresden, Germany<\/em><\/td><\/tr><tr><td>P4.9 Comparison of large eddy simulation models for arctic clouds<br>Tomi Raatikainen*<sup>1<\/sup>, Jaakko Ahola<sup>1<\/sup>, Juha Tonttila<sup>2<\/sup>, Sami Romakkaniemi<sup>2<\/sup>, Ari Laaksonen<sup>1<\/sup>, Hannele Korhonen<sup>1<\/sup><br><em><sup>1<\/sup><\/em><em>Finnish Meteorological Institute, Finland, <sup>2<\/sup>Finnish Meteorological Institute, Finland<\/em><\/td><\/tr><tr><td>P4.10 The Importance of Soil Dust for Mixed-phase Clouds in Global Climate Models<br>Luisa Ickes*, Tanja Stanelle, Ulrike Lohmann<br><em>Institute for Atmospheric and Climate Science, Switzerland<\/em><\/td><\/tr><tr><td>P4.11 Aircraft measurements of&nbsp; mixed-phase clouds versus cloud-resolving modeling studies in Northern China<br>Xueliang Guo*, Shichao Zhu, Guangxian Lu, Lijun Guo<br><em>Chinese Academy of Meteorological Sciences, China<\/em><\/td><\/tr><tr><td>P4.12 Formation and development of orographic mixed phase clouds in real cases<br>Olga Henneberg*, Ulrike Lohmann, Jan Henneberger<br><em>ETH Zurich, Switzerland<\/em><\/td><\/tr><tr><td>P4.13 An LES study on the role of ship induced ACI in mixed-phase stratocumulus<br>Anna Possner*<sup>1<\/sup>, Annica Ekman<sup>2<\/sup>, Ulrike Lohmann<sup>1<\/sup><br><em><sup>1<\/sup><\/em><em>ETH Zurich, Switzerland, <sup>2<\/sup>Stockholm University, Sweden<\/em><\/td><\/tr><tr><td>P4.14 The evolution and precipitation production of an orographic wintertime cloud with freezing drizzle<br>Sarah Tessendorf*<sup>1<\/sup>, Jeffrey French<sup>2<\/sup>, Courtney Weeks<sup>1<\/sup>, Roy Rasmussen<sup>1<\/sup>, Bart Geerts<sup>2<\/sup>, Binod Pokharel<sup>2<\/sup>, Lulin Xue<sup>1<\/sup>, Pat Holbrook<sup>3<\/sup>, Derek Blestrud<sup>3<\/sup>, Melvin Kunkel<sup>3<\/sup>, Shaun Parkinson<sup>3<\/sup><br><em><sup>1<\/sup><\/em><em>NCAR\/RAL, USA, <sup>2<\/sup>University of Wyoming, USA, <sup>3<\/sup>Idaho Power Company, USA<\/em><\/td><\/tr><tr><td>P4.15 Modelling of water stable isotope ratios in a 1.5D bin-resolved microphysics model<br>Andrea Flossmann*<sup>1,2<\/sup>, Wolfram Wobrock<sup>1,2<\/sup><br><em><sup>1<\/sup><\/em><em>LaMP\/UBP, France, <sup>2<\/sup>INSU\/CNRS, France<\/em><\/td><\/tr><tr><td>P4.16 Ground based in situ measurements of arctic cloud microphysical and optical properties at Mount Zeppelin, Svalbard<br>Guyot gwennol\u00e9*<sup>1<\/sup>, Jourdan Olivier<sup>1<\/sup>, Olofson Frans<sup>1<\/sup>, Schwarzenboeck Alfons<sup>1<\/sup>, Gourbeyre Christophe<sup>1<\/sup>, Febvre Guy<sup>1<\/sup>, Dupuy R\u00e9gis<sup>1<\/sup>, Bernard Christophe<sup>2<\/sup>, Tunved Peter<sup>3<\/sup>, Ancellet G\u00e9rard<sup>4<\/sup>, Law Kathy<sup>4<\/sup>, Wobrock Wolfram<sup>1<\/sup>, Shcherbakov Valery<sup>1<\/sup><br><em><sup>1<\/sup><\/em><em>LaMP, France, <sup>2<\/sup>OPGC, France, <sup>3<\/sup>Department of Applied Environmental Science, Sweden, <sup>4<\/sup>LATMOS, France<\/em><\/td><\/tr><tr><td>P4.17 Identification of super-cooled liquid layers in mixed-phase clouds based on cloud radar observations<br>Anne Hirsikko<sup>1<\/sup>, Ewan O&#8217;Connor<sup>1,2<\/sup>, Mika Komppula<sup>3<\/sup>, Sami Romakkaniemi*<sup>3<\/sup><br><em><sup>1<\/sup><\/em><em>Finnish Meteorological Institute, Finland, <sup>2<\/sup>University of Reading, UK, <sup>3<\/sup>Finnish Meteorological Institute, Finland<\/em><\/td><\/tr><tr><td>P4.18 Understanding microphysical controls on arctic stratus clouds: A comparison of high-resolution NWP models during the ASCOS field campaign<br>Christopher Dearden*<sup>1<\/sup>, Robin Stevens<sup>2<\/sup>, Anna Possner<sup>3<\/sup><br><em><sup>1<\/sup><\/em><em>University of Manchester, UK, <sup>2<\/sup>University of Leeds, UK, <sup>3<\/sup>ETH, Switzerland<\/em><\/td><\/tr><tr><td>P4.19 Response of mixed-phase boundary layer clouds with predominantly rapid or slow ice nucleation processes to cloud-top temperature trend<br>Ann Fridlind*<sup>1<\/sup>, Alexander Avramov<sup>2<\/sup>, Andrew Ackerman<sup>1<\/sup>, Peter Alpert<sup>3<\/sup>, Daniel Knopf<sup>4<\/sup>, Paul DeMott<sup>5<\/sup>, Sarah Brooks<sup>6<\/sup>, Andrew Glen<sup>6<\/sup><br><em><sup>1<\/sup><\/em><em>NASA GISS, USA, <sup>2<\/sup>MIT, USA, <sup>3<\/sup>CNRS, France, <sup>4<\/sup>Stony Brook University, USA, <sup>5<\/sup>Colorado State University, USA, <sup>6<\/sup>Texas A&amp;M University, USA<\/em><\/td><\/tr><tr><td>P4.20 A model for a turbulent mixed-phase cloud<br>Ben Devenish<br><em>Met Office, UK<\/em><\/td><\/tr><\/tbody><\/table><\/figure>\n","protected":false},"excerpt":{"rendered":"<p>Oral session: S4.1 Microphysical cloud properties and cloud probes&#8217; benchmark during the Pallas Cloud Experiments (PaCE).Konstantinos Doulgeris*1, Ari Leskinen2, Mika Komppula2, David Brus11Finnish Meteorological Institute, Finland, 2Finnish Meteorological Institute, Finland (video; position 0:00) S4.2 Liquid water content and effective radius retrievals in mixed-phase cloud layers from Cloud radar data based on the forward modelingYujun Qiu*1, [&hellip;]<\/p>\n","protected":false},"author":9,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"ngg_post_thumbnail":0,"cybocfi_hide_featured_image":"","footnotes":""},"class_list":["post-617","page","type-page","status-publish","hentry"],"post_mailing_queue_ids":[],"_links":{"self":[{"href":"https:\/\/www.iamas.org\/iccp\/wp-json\/wp\/v2\/pages\/617","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.iamas.org\/iccp\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/www.iamas.org\/iccp\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/www.iamas.org\/iccp\/wp-json\/wp\/v2\/users\/9"}],"replies":[{"embeddable":true,"href":"https:\/\/www.iamas.org\/iccp\/wp-json\/wp\/v2\/comments?post=617"}],"version-history":[{"count":3,"href":"https:\/\/www.iamas.org\/iccp\/wp-json\/wp\/v2\/pages\/617\/revisions"}],"predecessor-version":[{"id":672,"href":"https:\/\/www.iamas.org\/iccp\/wp-json\/wp\/v2\/pages\/617\/revisions\/672"}],"wp:attachment":[{"href":"https:\/\/www.iamas.org\/iccp\/wp-json\/wp\/v2\/media?parent=617"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}