<?xml version="1.0" encoding="UTF-8"?><resource xsi:schemaLocation="http://datacite.org/schema/kernel-4 http://schema.datacite.org/meta/kernel-4.3/metadata.xsd" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xmlns="http://datacite.org/schema/kernel-4"><identifier identifierType="DOI">10.1594/PANGAEA.666164</identifier><creators><creator><creatorName>Grassl, Hartmut</creatorName><givenName>Hartmut</givenName><familyName>Grassl</familyName></creator></creators><titles><title>Radiation balance of the tropical ocean surface measured during Atlantic Expedition GARP 1974 (Table 1)</title></titles><publisher>PANGAEA</publisher><publicationYear>1977</publicationYear><subjects><subject subjectScheme="Parameter">DATE/TIME</subject><subject subjectScheme="Parameter">ALTITUDE</subject><subject subjectScheme="Parameter">Short-wave downward (GLOBAL) radiation</subject><subject subjectScheme="Parameter">Short-wave upward (REFLEX) radiation</subject><subject subjectScheme="Parameter">Long-wave downward radiation</subject><subject subjectScheme="Parameter">Long-wave upward radiation</subject><subject subjectScheme="Method">Observation</subject><subject subjectScheme="Campaign">PL9/74</subject><subject subjectScheme="Basis">Planet II (1967-2004)</subject></subjects><dates><date dateType="Collected">1974-08-31T00:00:00/1974-09-18T00:00:00</date></dates><resourceType resourceTypeGeneral="Dataset">Supplementary Dataset</resourceType><sizes><size>69 data points</size></sizes><formats><format>text/tab-separated-values</format></formats><rightsList><rights rightsURI="https://creativecommons.org/licenses/by/3.0/" schemeURI="https://spdx.org/licenses/" rightsIdentifierScheme="SPDX" rightsIdentifier="CC-BY-3.0">Creative Commons Attribution 3.0 Unported</rights></rightsList><descriptions><description descriptionType="Abstract">The net flux of all irreversible fluxes of radiation and heat crossing the ocean surface is determined for phase III of GATE at position no. 27 (WFS "Planet", FRG). The radiation fluxes have been measured directly, while the heat fluxes have been parameterized with the bulk formula however with bulk coefficients depending on stability. The heat loss of the ocean due to warming of the cooler precipitation is included for the determination of the net flux at the ocean surface. Some examples of hourly mean values of different fluxes during different weather conditions are additionally shown.</description><description descriptionType="Other">Supplement to: Grassl, Hartmut (1977): Gemessene Strahlungs- und Wärmeflüsse über dem tropischen Ozean (Measured radiation and heat fluxes at the tropical ocean surface). Meteor Forschungsergebnisse, Deutsche Forschungsgemeinschaft, Reihe B Meteorologie und Aeronomie, Gebrüder Bornträger, Berlin, Stuttgart, B12, 42-50</description></descriptions><geoLocations><geoLocation><geoLocationPoint><pointLongitude>-23.0</pointLongitude><pointLatitude>9.75</pointLatitude></geoLocationPoint></geoLocation><geoLocation><geoLocationPlace>Atlantic</geoLocationPlace></geoLocation></geoLocations></resource>