Large climate-induced changes in ultraviolet index and stratosphere-to-troposphere ozone flux

By M. Hegglin, T. G. Shepherd. 2009

284 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/342374acfa0f226ba1a4f8477d1066a06f3e8000

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Atmospheric Science

1. William J. Randel
2. M. Hegglin
3. T. Birner
4. T. G. Shepherd
5. L. Pan
6. Andrew Gettelman
7. C. McLandress
8. P. Hoor

In Global and Planetary Change

1. William J. Randel
2. T. Birner
3. M. Hegglin
4. T. G. Shepherd
5. L. Pan
6. Andrew Gettelman
7. G. Myhre
8. C. McLandress

Citations in the corpus

• Effects of N supply on the accumulation of photosynthetic pigments and photoprotectors in Gracilaria tenuistipitata (Rhodophyta) cultured under UV radiation (2011, background): “During the last decades, ultraviolet radiation (UVR) has increased over the Earth surface, and there are predictions for further increase, mainly in tropical zones ( Hegglin and Sheperd 2009; Li et al. 2009).”
• A Robust Mechanism for Strengthening of the Brewer–Dobson Circulation in Response to Climate Change: Critical-Layer Control of Subtropical Wave Breaking (2011, background): “Rind et al. (1990) also suggested that the ozone redistribution would affect the penetration of UV radiation into the troposphere, which was confirmed by Hegglin and Shepherd (2009).”
• The future of seaweed aquaculture in a rapidly changing world (2017, background): “…breakdown of stratospheric ozone and global warming and, although ozone ‘holes’ are still occurring annually over the Poles, increases in UVB fluxes to the Earth’s surface are not restricted to high latitudes, though changes at the tropics are minimal (Hegglin & Shepherd, 2009; Herman, 2010).”
• THE EXTRATROPICAL UPPER TROPOSPHERE AND LOWER STRATOSPHERE (2011, background): “By the end of the 21st century, climate change is predicted to substantially change UTLS ozone distributions through changes in stratospheric transport, with a potentially strong feedback on radiative forcing and STE [ Hegglin and Shepherd , 2009].”
• Anthropogenic and Natural Radiative Forcing (2014, background): “Additional model estimates of this influx (Hegglin and Shepherd, 2009; Hsu and Prather, 2009) fall within both ranges, as do estimates based on observations (Murphy and Fahey, 1994; Gettelman et al.”