Az IPCC a légköri vizet a climate feedback kategóriába rakja, amivel az olyan outsidereket, mint te is vagy, jól megzavarja, ezért nem találod az adatokat.
Akkor idézném a legutóbbi IPCC jelentés draftjának idevonatkozó részeit:
"10 The magnitude of global surface temperature change primarily depends on the strength of the radiative
11 forcings and feedbacks, the latter defined as the changes of the net energy budget at the top of atmosphere
12 (TOA) in response to a change in the GSAT (Box 7.1, Equation 7.1). Feedbacks in the Earth system are
13 numerous, and it can be helpful to categorise them into three groups: (1) physical feedbacks; (2)
14 biogeophysical and biogeochemical feedbacks; and (3) long-term feedbacks associated with ice sheets. The
15 physical feedbacks (for example, associated with changes in lapse-rate, water vapour, surface albedo, or
16 clouds; Sections 7.4.2.1-7.4.2.4) and biogeophysical/biogeochemical feedbacks (for example, associated
17 with changes in methane, aerosols, ozone, or vegetation; Section 7.4.2.5) act both on time scales that are
18 used to estimate the equilibrium climate sensitivity (ECS) in models (typically 150 years, see Box 7.1) and
19 on longer time scales required to reach equilibrium. Long-term feedbacks associated with ice sheets (Section
20 7.4.2.6) are relevant primarily after several centuries or more. The feedbacks associated with
21 biogeophysical/biogeochemical processes and ice sheets, often collectively referred to as Earth system
22 feedbacks, had not been included in conventional estimates of the climate feedback (e.g., Hansen et al.,
23 1984), but the former can now be quantified and included in the assessment of the total (net) climate
24 feedback. Feedback analysis represents a formal framework for the quantification of the coupled interactions
25 occurring within a complex Earth system in which everything influences everything else (e.g., Roe, 2009).
26 As used here and presented in Section 7.4.1, its primary objective is to identify and understand the key
27 processes that determine the magnitude of the surface temperature response to an external forcing. For each
28 feedback, the basic underlying mechanisms and their assessment are presented in Section 7.4.2."
"30 Up until AR5, process understanding and quantification of feedback mechanisms were based primarily on
31 global climate models. Since AR5, the scientific community has undertaken a wealth of different alternative
32 approaches, including observational and fine-scale modelling approaches. This has in some cases led to more
33 constrained feedbacks and, on the other hand, uncovered shortcomings in global climate models, which are
34 starting to be corrected. Consequently, AR6 achieves a more robust assessment of feedbacks in the climate
35 system that is less reliant on global climate models than in earlier assessment reports." 1673. oldal
"54 Greater atmospheric water vapour content,
54 particularly in the upper troposphere, results in enhanced absorption of LW and SW radiation and reduced
55 outgoing radiation. This is a positive feedback. Atmospheric moistening has been detected in satellite records
1 (Chapter 2, Section 2.3.1.3.3), is simulated by climate models (Chapter 3, Section 3.3.2.1), and the estimates
2 agree within model and observational uncertainty (Soden et al., 2005; Dessler, 2013; Gordon et al., 2013;
3 Chung et al., 2014). The estimate of this feedback inferred from satellite observations is αWV = 1.85 ± 0.32
4 W m–2 °C–1 (Liu et al., 2018). This is consistent with the value αWV = 1.77 ± 0.20 W m–2 °C–1 (one standard
5 deviation) obtained with CMIP5 and CMIP6 models (Zelinka et al., 2020). 1674-1675. oldal
Köszönő viszonyban sincs az általad írt semleges hatással, vagy az általad megadott értékkel.
Szal, akkor most a sajátodon kívül milyen álláspontot fogadsz el, csak mert az IPCC adatait sem ismered?!