Revisiting the Agung 1963 volcanic forcing – impact of one or two eruptions by U. Niemeier, C. Timmreck, K. Krüger

“…The two smaller eruptions result in a lower sulfur burden, smaller aerosol particles, and 0.1 to 0.3&thinsp;<span class="inline-formula">Wm⁻²</span> (10&thinsp;%–20&thinsp;%) lower radiative forcing in monthly mean global average compared to the individual eruption experiment. …”
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Climate Influence in Dendrochronological Series of <i>Araucaria angustifolia</i> from Campos do Jordão, Brazil by Daniela Oliveira da Silva, Alan Prestes, Virginia Klausner, Táyla Gabrielle Gonçalves de Souza

“…We obtained correlations as high as <inline-formula><math xmlns="http://www.w3.org/1998/Math/MathML" display="inline"><semantics><mrow><mi>r</mi><mo>=</mo><mn>0.22</mn><mspace width="0.277778em"></mspace><mo>(</mo><mi>α</mi><mo>=</mo><mn>0.1</mn><mo>)</mo></mrow></semantics></math></inline-formula> for precipitation (February), and <inline-formula><math xmlns="http://www.w3.org/1998/Math/MathML" display="inline"><semantics><mrow><mi>r</mi><mo>=</mo><mn>0.21</mn><mspace width="0.277778em"></mspace><mo>(</mo><mi>α</mi><mo>=</mo><mn>0.1</mn><mo>)</mo></mrow></semantics></math></inline-formula> for temperature (March), both corresponding to the end of the summer season. …”
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Low-flow estimation beyond the mean – expectile loss and extreme gradient boosting for spatiotemporal low-flow prediction in Austria by J. Laimighofer, M. Melcher, G. Laaha

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Regional, multi-decadal analysis on the Loire River basin reveals that stream temperature increases faster than air temperature by H. Seyedhashemi, H. Seyedhashemi, J.-P. Vidal, J. S. Diamond, D. Thiéry, C. Monteil, F. Hendrickx, A. Maire, F. Moatar

“…</p> <p>Stream temperature increased for almost all reaches in all seasons (mean <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M3" display="inline" overflow="scroll" dspmath="mathml"><mrow><mo>=</mo><mo>+</mo><mn mathvariant="normal">0.38</mn></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="41pt" height="10pt" class="svg-formula" dspmath="mathimg" md5hash="a399da75d82899c4566cd46dd86a5d8b"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="hess-26-2583-2022-ie00001.svg" width="41pt" height="10pt" src="hess-26-2583-2022-ie00001.png"/></svg:svg></span></span> <span class="inline-formula">^∘</span>C decade<span class="inline-formula">−1</span>) over the 1963–2019 period. …”
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Surface temperature response to the major volcanic eruptions in multiple reanalysis data sets by M. Fujiwara, P. Martineau, J. S. Wright

“…<p>The global response of air temperature at 2&thinsp;m above the surface to the eruptions of Mount Agung in March 1963, El Chichón in April 1982, and Mount Pinatubo in June 1991 is investigated using 11 global atmospheric reanalysis data sets (JRA-55, JRA-25, MERRA-2, MERRA, ERA-Interim, ERA-40, CFSR, NCEP-NCAR R-1, 20CR version 2c, ERA-20C, and CERA-20C). …”
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