Sandro Veiga

Dr. Sandro Veiga


Research Focus & Metrics

Academic Career Length

6Years (2021-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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23 September 2023 in Scientific Reports
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Journal Article
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PNPaulo Nobre
Paulo Nobre
SVSandro Veiga
Sandro Veiga
EGEmanuel Giarolla
Emanuel Giarolla
AMAndre Lanfer Marquez
Andre Lanfer Marquez
MSManoel B. da Silva
Manoel B. da Silva
CNCARLOS AFONSO NOBRE
CARLOS AFONSO NOBRE
This study presents novel insight into the mechanisms of Atlantic Meridional Overturning Circulation (AMOC) reduction and its recovery under a warmer climate scenario. An one-thousand-year-long numerical simulation of a global coupled ocean–ice–atmosphere climate model, subjected to a stationary atmospheric radiative forcing, depict a coherent picture of the Arctic sea ice melting as a trigger for the initial AMOC reduction, along with decreases in the northward fluxes of salt and heat. Further atmospheric-driven ocean processes contribute to an erosion of the stable stratification of the fresher, yet colder waters in the surface layers of the North Atlantic, contributing to the recovery of a permanently altered AMOC.

31 January 2023 in Theoretical and Applied Climatology
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Journal Article
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WFWendell M. B. Fialho
Wendell M. B. Fialho
LCLeila Carvalho
Leila Carvalho
MGManoel Alonso Gan
Manoel Alonso Gan
SVSandro Veiga
Sandro Veiga

16 September 2023 in Journal of South American Earth Sciences
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Journal Article
Closed access
SVSandro Veiga
Sandro Veiga
PNPaulo Nobre
Paulo Nobre
EGEmanuel Giarolla
Emanuel Giarolla
VCVinícius B. Capistrano
Vinícius B. Capistrano
MSManoel B. da Silva
Manoel B. da Silva
CNCarlos A. Nobre
Carlos A. Nobre

1 December 2021 in Weather and Climate Extremes
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Journal Article
Open access
SVSandro Veiga
Sandro Veiga
HYHuiling Yuan
Huiling Yuan

19 April 2024 in Climate Dynamics
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Journal Article
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SVSandro Veiga
Sandro Veiga
HYHuiling Yuan
Huiling Yuan

14 March 2026
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Conference Paper
Open access
SVSandro Veiga
Sandro Veiga
HYHuiling Yuan
Huiling Yuan
Sea turtles are among the marine life endangered by human activities that directly disturb their environment, such as fisheries bycatch, habitat degradation, and pollution. Additionally, the effects of ongoing global warming can also pose an extra threat since sea turtles are a species with temperature-dependent sex determination. Hence, with the increasing temperatures, they may experience a feminization phenomenon that can pose a risk to their extinction. Since the female sea turtles exhibit a great fidelity to beach sites where they were nested, a potential behavioral change to mitigate the effects of global warming is a nesting phenological shift to cooler periods of the year. Based on previous observations, the most optimistic phenological shift for sea turtles can be extrapolated to 27 days (about one month) per 1.5°C increase in the nesting sand temperature. Using this hypothesis, in this study, we aim to assess by when the sea turtles have to perform a one-month phenological shift in 48 sites around the world and the respective warming mitigation achieved by the phenological shift. We used two future climate scenarios (SSP2-4.5 and SSP5-8.5) from the simulations of 22 CMIP6 climate models. For SSP2-4.5 future scenario (a moderate scenario), it is projected that the middle of this century is the earliest date for phenological shift in sites located in the southeastern part of the USA and in the eastern Mediterranean sites. Sea turtles nesting in the equatorial sites have up to the end of the century or beyond to perform a phenological shift. However, the warming mitigation is greater in sites located further away from the equatorial region, whereas the sites in the equatorial region show a small mitigation effect from the phenological shift. Regarding the SSP5-8.5 future scenario (an extreme scenario), the phenological shift has to be performed in this century in all sites, with some sites in the Mediterranean with threshold dates sooner than mid-21th century. Moreover, compared with the SSP2-4.5 future scenario, there is some reduction in warming mitigation capacity, but it is not significantly different from the moderate scenario. Considering the uncertainty from the climate models' projections, our analysis shows that the models have lower uncertainty in sites projecting earlier threshold dates for phenological shifts.