What experiments are scientists doing about global warming?

Many issues will arise from global climate change (not global warming). Scientists are working to create new ways to adapt to these changes. One is the use of genetically modified organisms (GMOs), which will be able to survive in arid or hotter environments (compared to the good old days).

Another is altering the plant cover of a region. Certain regions will likely be severely affected in the future (perhaps becoming arid or extremely hot), while other regions have already experienced these conditions. Certain species can spread to new areas.

Due to global climate change, tourism will be a good industry in northern regions (not in the Mediterranean) like the Nordic countries or Ukraine.

A number of scientists monitor plants or other species that are under stress due to climate change. Reporting on future conditions is another aspect of their work.

For a more thorough response, you can go to the websites listed below:

Bernd-BlumeExperiments.pdf can be found at https://tutor.hix.ai

globalwarming.html https://tutor.hix.ai

The global warming experiment from 2009 to 2011 years is available as a PDF file at https://tutor.hix.ai

Although there are figures with temperature dimensions that attempt to do so, it is very difficult to even agree upon a definition of what constitutes "the" temperature of the Earth, let alone measure it currently, estimate it in the past, or predict it in the future.

For instance, estimates of the surface temperature every few degrees of latitude and longitude are the basis for the widely used Global Land-Ocean Temperature Index.

The Top of Lower Atmosphere is utilized by other researchers, particularly in satellite measurements (which rely on radiation from the lower atmosphere instead of the surface).

For example, sea temperatures are estimated from canvas buckets on sailing vessels, through engine cooling water intake on diesel engines, through free-floating buoys specifically designed for the purpose, and then to deep-sea submersible buoys. Air temperatures are measured with balloons. Determining whether there has been warming or cooling since, say, 1800 is challenging due to the scarcity of surface temperatures in the 1800s and the gradual change in temperature measuring procedures.

Satellites have made it possible to estimate surface temperatures over large regions to within a degree or two since about 1979, adding to the measurements taken using thermometers at weather stations dating back to about 1880.

A contentious area is the need to adjust the raw data to compensate for consistent changes in measurement procedures, particularly when estimating sea-surface temperatures in the 1800s, which are crucial because the amount of warming from the end of the Little Ice Age to the present is about half a degree Celsius. It is difficult to get temperature estimates with any of these procedures to within better than a degree of random error.

It becomes even more difficult to go back in time before thermometers and weather-station logging were commonplace. This is where "proxies" come in, items that are sensitive to temperature and can be used to "record" temperature in the past. These can be physical (like ice cores taken from the poles) or biological (like tree rings or other plant features and population densities).

Scientists are conducting various experiments related to global warming, including research on climate models, carbon capture and storage technologies, renewable energy sources, geoengineering techniques, and sustainable land management practices. Additionally, studies are underway to investigate the impacts of global warming on ecosystems, biodiversity, weather patterns, and human health, as well as potential mitigation and adaptation strategies.