<?xml version="1.0" encoding="UTF-8"?><!--*** Generated from internal PANGAEA metadata schema by dif.xslt ***--><DIF xsi:schemaLocation="http://gcmd.gsfc.nasa.gov/Aboutus/xml/dif/ http://gcmd.gsfc.nasa.gov/Aboutus/xml/dif/dif_v9.4.xsd" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xmlns="http://gcmd.gsfc.nasa.gov/Aboutus/xml/dif/">
<Entry_ID>PANGAEA_905102</Entry_ID>
<Entry_Title>Peroxy Radical Autoxidation Mechanism (PRAM)</Entry_Title>
<Data_Set_Citation>
<Dataset_Creator>Roldin, Pontus</Dataset_Creator>
<Dataset_Title>Peroxy Radical Autoxidation Mechanism (PRAM)</Dataset_Title>
<Dataset_Release_Date>2019-08-20</Dataset_Release_Date>
<Dataset_Publisher>PANGAEA</Dataset_Publisher>
<Data_Presentation_Form>Dataset</Data_Presentation_Form>
<Other_Citation_Details>Supplement to: Roldin, Pontus; Ehn, Mikael; Kurtén, Theo; Olenius, Tinja; Rissanen, Matti P; Sarnela, Nina; Elm, Jonas; Rantala, Pekka; Hao, Liqing; Hyttinen, Noora; Heikkinen, Liine; Worsnop, Douglas R; Pichelstorfer, Lukas; Xavier, Carlton; Clusius, Petri; Öström, Emilie; Petäjä, Tuukka; Kulmala, Markku; Vehkamäki, Hanna; Virtanen, Annele; Riipinen, Ilona; Boy, Michael (2019): The role of highly oxygenated organic molecules in the Boreal aerosol-cloud-climate system. Nature Communications, 10(1), https://doi.org/10.1038/s41467-019-12338-8</Other_Citation_Details>
<Online_Resource>https://doi.pangaea.de/10.1594/PANGAEA.905102</Online_Resource>
</Data_Set_Citation>
<Personnel>
<Role>Investigator</Role>
<First_Name>Pontus</First_Name>
<Last_Name>Roldin</Last_Name>
</Personnel>
<Discipline>
<Discipline_Name>Earth Science</Discipline_Name>
</Discipline>
<Parameters>
<Detailed_Variable>File content</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>File name</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>File format</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>File size</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>Uniform resource locator/link to file</Detailed_Variable>
</Parameters>
<ISO_Topic_Category>geoscientificInformation</ISO_Topic_Category>
<Keyword>Highly Oxygenated organic Molecules</Keyword>
<Keyword>Peroxy radical autoxidation</Keyword>
<Data_Set_Progress>Complete</Data_Set_Progress>
<Access_Constraints>unrestricted</Access_Constraints>
<Use_Constraints>CC-BY-4.0: Creative Commons Attribution 4.0 International</Use_Constraints>
<Data_Set_Language>English</Data_Set_Language>
<Data_Center>
<Data_Center_Name>
<Short_Name>PANGAEA</Short_Name>
<Long_Name>Data Publisher for Earth &amp; Environmental Science</Long_Name>
</Data_Center_Name>
<Data_Center_URL>https://www.pangaea.de/</Data_Center_URL>
<Personnel>
<Role>Data Center Contact</Role>
<First_Name>Michael</First_Name>
<Last_Name>Diepenbroek</Last_Name>
<Email>info@pangaea.de</Email>
<Contact_Address>
<Address>Leobener Str.</Address>
<City>Bremen</City>
<Province_or_State>Bremen</Province_or_State>
<Postal_Code>28359</Postal_Code>
<Country>Germany</Country>
</Contact_Address>
</Personnel>
</Data_Center>
<Distribution>
<Distribution_Media>online</Distribution_Media>
<Distribution_Size>15 data points</Distribution_Size>
<Distribution_Format>text/tab-separated-values</Distribution_Format>
</Distribution>
<Summary>Peroxy radical autoxidation mechanism (PRAM) for monoterpenes reacting with ozone or OH. PRAM should be coupled to the Master  Chemical Mechanism version 3.3.1 (MCMv3.3.1) or a similar chemical mechanism which calculates the peroxy radical (RO2) pool. ** For all details see the full metadata description at "https://doi.pangaea.de/10.1594/PANGAEA.905102"! ** The dataset contains three files:
1. PRAM_KPP
2. PRAMreduced_KPP
3. PRAM_species_properties</Summary>
<Related_URL>
<URL>https://doi.org/10.1038/s41467-019-12338-8</URL>
<Description>The role of highly oxygenated organic molecules in the Boreal aerosol-cloud-climate system</Description>
</Related_URL>
<Metadata_Name>DIF</Metadata_Name>
<Metadata_Version>9.4</Metadata_Version>
<DIF_Creation_Date>2019-08-20</DIF_Creation_Date>
<Last_DIF_Revision_Date>2026-04-30</Last_DIF_Revision_Date>
</DIF>
