<ref xmlns="http://www.tei-c.org/ns/1.0" xml:id="be99db3d-2457-4058-99db-3d24571058a4" corresp="#e9f2ab90-afba-41f0-b2ab-90afba91f0d5" type="editorialNote"> <bibl corresp="https://edition-humboldt.de/8N8XBR7Q"><persName ref="https://edition-humboldt.de/H0006198 http://d-nb.info/gnd/117560952"> <choice> <abbr>Wahlenb.</abbr> <expan>Wahlenberg</expan> </choice></persName><supplied cert="high">,</supplied> <lb /> <choice> <abbr>Helv.</abbr> <expan>Helvetia</expan> </choice><supplied cert="high">,</supplied> <choice> <abbr>p</abbr> <expan>page</expan> </choice> <lb />LXXXV</bibl> </ref><note xmlns="http://www.tei-c.org/ns/1.0" xml:id="e9f2ab90-afba-41f0-b2ab-90afba91f0d5" corresp="#be99db3d-2457-4058-99db-3d24571058a4" type="editorial" resp="#UL"> <quote>Jam supra […] calorem-solarem reflexum vel potius inclusum quodammodo adumbravimus, qui e differentia temperaturae nocturnae et diurnae cognoscitur et eo major existimatur quo serius post culminationem solis accedit, qui major esse videtur in terris australioribus ubi sol alte adscendit, et qui in vallibus inclusis regnat et ad loca umbrosa adeo extenditur, ut eum ex observationibus suis in umbra factis excludere non possint Physici, ideoque speciali adumbratione haud indigeat. Nunc autem quaedam adferre necesse est de calore solari directo, qui e differentia inter temperaturam in luce solari et in umbra aestimatur, qui in terris campestribus et maritimis major est, et qui eo magis insignis esse videtur quo minus sol in coelum elevatur, ideoque in terris borealibus efficacior fit, et quem omni successu ex observationibus suis excludunt Physici adeo ut speciali consideratione omnino indigeat.</quote> <bibl corresp="https://edition-humboldt.de/8N8XBR7Q">Wahlenberg 1813</bibl>, LXXXV.</note>