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<blockquote style="position: relative; padding-left: 55px;"><section><a href="https://rollenspiel.social/users/ArneBab/statuses/113516468268274496">Arne Babenhauserheide (arnebab@rollenspiel.social)'s status on Thursday, 21-Nov-2024 02:30:47 JST</a><a href="https://rollenspiel.social/@ArneBab" title="arnebab@rollenspiel.social"><img src="https://gnusocial.jp/avatar/8121-48-20230128222518.webp" width="48" height="48" alt="Arne Babenhauserheide" style="position: absolute; left: 0; top: 0;">Arne Babenhauserheide</a><div><a href="https://gruene.social/@herdsoft/113516386826596545" rel="in-reply-to">in reply to</a><ul><li></ul></div></section><article><p><a href="https://gruene.social/@herdsoft">@herdsoft</a> ich habe die Daten gefunden, weil ich mir genau die Frage auch gestellt habe.</p><p>Methan scheint sqrt zu sein: <a href="https://en.wikipedia.org/wiki/Radiative_forcing#Other_trace_gases" rel="nofollow noreferrer">https://en.wikipedia.org/wiki/Radiative_forcing#Other_trace_gases</a></p><p>⇒ am Ende muss man doch immer konkret auf Zahlen schauen, um zu wissen, was relevant ist.</p></article><footer><a rel="bookmark" href="https://gnusocial.jp/conversation/3951625#notice-7887983">In conversation</a><time datetime="2024-11-21T02:30:47+09:00" title="Thursday, 21-Nov-2024 02:30:47 JST">about a day ago</time> <span>from <span><a href="https://rollenspiel.social/@ArneBab/113516468268274496" rel="external" title="Sent from rollenspiel.social via ActivityPub">rollenspiel.social</a></span></span><a href="https://rollenspiel.social/@ArneBab/113516468268274496">permalink</a><h4>Attachments</h4><ol><li><article><header><div>Domain not in remote thumbnail source whitelist: upload.wikimedia.org</div><h5><a href="https://en.wikipedia.org/wiki/Radiative_forcing#Other_trace_gases">Radiative forcing</a></h5><div></div></header><div>Radiative forcing (or climate forcing) is a concept used to quantify a change to the balance of energy flowing through a planetary atmosphere. Various factors contribute to this change in energy balance, such as concentrations of greenhouse gases and aerosols, and changes in surface albedo and solar irradiance. In more technical terms, it is defined as "the change in the net, downward minus upward, radiative flux (expressed in W/m2) due to a change in an external driver of climate change.": 2245  These external drivers are distinguished from feedbacks and variability that are internal to the climate system, and that further influence the direction and magnitude of imbalance. Radiative forcing on Earth is meaningfully evaluated at the tropopause and at the top of the stratosphere. It is quantified in units of watts per square meter, and often summarized as an average over the total surface area of the globe.
A planet in radiative equilibrium with its parent star and the rest of space can be characterized by net zero radiative forcing and by a planetary equilibrium temperature...</div><footer></footer></article></li></ol></footer></blockquote>

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Arne Babenhauserheide (arnebab@rollenspiel.social)'s status on Thursday, 21-Nov-2024 02:30:47 JSTArne Babenhauserheide
in reply to
- Bernd Herd
@herdsoft ich habe die Daten gefunden, weil ich mir genau die Frage auch gestellt habe.
Methan scheint sqrt zu sein: https://en.wikipedia.org/wiki/Radiative_forcing#Other_trace_gases
⇒ am Ende muss man doch immer konkret auf Zahlen schauen, um zu wissen, was relevant ist.
In conversationabout a day ago from rollenspiel.socialpermalink
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  Radiative forcing
  Radiative forcing (or climate forcing) is a concept used to quantify a change to the balance of energy flowing through a planetary atmosphere. Various factors contribute to this change in energy balance, such as concentrations of greenhouse gases and aerosols, and changes in surface albedo and solar irradiance. In more technical terms, it is defined as "the change in the net, downward minus upward, radiative flux (expressed in W/m2) due to a change in an external driver of climate change.": 2245 These external drivers are distinguished from feedbacks and variability that are internal to the climate system, and that further influence the direction and magnitude of imbalance. Radiative forcing on Earth is meaningfully evaluated at the tropopause and at the top of the stratosphere. It is quantified in units of watts per square meter, and often summarized as an average over the total surface area of the globe. A planet in radiative equilibrium with its parent star and the rest of space can be characterized by net zero radiative forcing and by a planetary equilibrium temperature...

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