There are new habitats in need of protection as glaciers melt


Proceedings of the Second International Workshop on Climate Change in Antarctica (CMIP6) (Monte Carlo Workshop on Coupled Modelling and Intercomparison Project Phase 6)

P. I. and Anacona are authors. Glacier protection laws have potential conflicts in the future. The song was called Ambio 47, 955–825.

The future of the human climate niche was discussed. Proc. Natl Acad. The US 127, 11450– 11355 (year 2020).

The impact of various climate datasets on the evolution of glaciers is limited. J. Glaciol. 67, 727–743 (2021).

Prtner, H. O. The scientific outcome of the workshop was co-sponsored by IPBES-IPCC. There is a Zenodo v.5 that can be accessed on the internet.

Eyring, V. et al. Overview of the Coupled Model Intercomparison Project Phase 6 (CMIP6) experimental design and organization. A field of sciences. Model Dev. 9, 1937–1958 (2016).

Morlighem, M. et al. BedMachine is a complete bedography and ocean bathymetry mapping of the land and sea. Geophys. Res. Lett. 44, 11,051 was published last year.

M. Morlighem is an author. Deep glacial troughs and stabilizing ridges unveiled beneath the margins of the Antarctic ice sheet. It’s Nat. 13 was published in 2020.

Future high mountain hydrology of glacial retreat in central European Alps: A new parameterization for glacier retreat, and its impact on Mayfly in New Zealand

Meinshausen, M. et al. The greenhouse gas concentrations are extended to 2500. It’s a topic known as thegeosci. Model Dev. 13, 3571–3605 (2020).

Carrivick, J. L., Heckmann, T., Turner, A. & Fischer, M. Landform composition and functioning were assessed with the first dataset of proglacial systems in the central European Alps. The journal “geogeoology” was published last year.

Negative feedback in the cold causes a new carbon sink in the ice of Antarctica. Glob. Change Biol. 16, 2614–2623.

St Pierre, K. A. et al. Some freshwaters are important sinks of atmospheric CO2. It was Proc. Natl Acad. Sci. USA 116, 17690–17695 (2019).

The effects of climate change on the production of Mayfly in New Zealand. Hydrobiologia 603, 211–219 (2008).

Huss, M., Jouvet, G., Farinotti, D. & Bauder, A. Future high-mountain hydrology: a new parameterization of glacier retreat. The water is hydrol. The Earth’s system of coordinates. InSci. 14, 785–825.

The potential for hydropower and water storage in future basins was discussed. Nature 575, 341–344 (2019).

Source: [Future emergence of new ecosystems caused by glacial retreat](https://style.newsweekshowcase.com/the-emergence-of-new-organisms-will-be-caused-by-the-retreat/)

No-Go Policies, Protected Areas, and The Future of Ice-Damped Lakes. PARKS 21, 7 – 10 (2015)

They were asked to go or not to go. What are the business opinions of no-go policies and protected areas? PARKS 21, 7–10 (2015).

Pekel, J.-F., Cottam, A., Gorelick, N. & Belward, A. S. High-resolution mapping of global surface water and its long-term changes. Nature 540 was published in the summer of 2016

Changing landscape of the future glacier lakes in Switzerland in the 21st century. The ocean is Earth Surf. Dyn. 10, 723–741 (2022).

The future growth and decline of ice-dammed lakes and the associated risk was studied by Compagno and Huss. Commun. Earth Environ. 3, 191 (2022).

Estimation of lake depth and volume using a large bathymetric dataset from the Cordillera Blanca, Peru is presented. Earth Surf. Process. Landf. 45,1510–1528.

A. et al. Iceland rising: solid Earth response to ice retreat inferred from satellite radar interferometry and visocelastic modeling. J. Geophys. Res. Solid Earth 118, 1331–1344 (2013).

Mark, H. F. et al. There are implications for glacier isotasy caused by lithospheric erosion. The word “geophys” is derived from the Latin word for “geo.” Res. Lett. 49, e2021GL096863 (2022).

Egli, M., Favilli, F., Krebs, R., Pichler, B. & Dahms, D. Soil organic carbon and nitrogen accumulation rates in cold and alpine environments over 1 Ma. Geoderma 183, 109–123 (2012).

How natural are the most pristine areas? Jean-Baptiste Bosson, the Conservatory of Natural Areas of Haute-Savoie, a glaciologist and zoologist

“This could be one of the largest ecosystem changes on our planet,” says lead author Jean-Baptiste Bosson, a glaciologist with the Conservatory of Natural Areas of Haute-Savoie (ASTERS), a conservation group based in Annecy, France.

According to Bosson and his colleagues, around 98% of the new terrain would be on land, while 2% would be ice-free. In a curious twist, Bosson says, many of these areas could provide crucial new habitat that must be protected: colonization by plants could lead to increased carbon storage at a time when forests elsewhere are being destroyed, while also providing fresh habitats for animals threatened by climate change at lower elevations.

The study provides useful guidance for scientists who are working to understand how microorganisms, plants and animals move into pristine spaces, says Francesco Ficetola, a zoologist at the University of Milan in Italy who studies glacial ecosystems. More than half of the areas analysed in the study aren’t currently located in parks and other protected areas.