I believe the correct answer from the choices listed above is the second option. In the summer, temperatures exceed 100 f, whether it's a cloudy day or clear day. The seasonal weather condition expressed here is the summer. It <span>is the hottest of the four temperate seasons, falling between spring and autumn.</span>
Global warming impacts terrestrial biomes since it brings about <span>decreased precipitation and longer winter seasons. Global warming refers to the increase in temperature of the Earth's atmosphere. This is brought about by release of greenhouse gases (e.g. carbon dioxide, methane) in the air which trap heat in the Earth's atmosphere. As a result, there is increased variability of weather and climate patterns. </span>
Answer:
Farming/rotational grazing
Explanation:
Right, so it's 9pm where I'm at right now and I'm exhausted from writing all day, so this answer's gonna be really brief. I hope you don't mind and that it's at least somewhat helpful.
Global warming is just a side effect of a much larger problem, which is climate change. Climate change is when some areas get hotter and some areas colder because of the disrupted weather patterns. It can't be stopped, because the climate will fluctuate over time. What can be changed is how extreme these changes are. Today human beings are not the cause of climate change, but we are contributing to it from all the gases we release into the air.
An unexpected - but possible - solution could lie in effective horticulture. Search up "Scott Strough Red Baron Project".
What Mr. Strough's project aims to do essentially is grow plants and nurture soil in such a way that carbon can be sucked from the atmosphere. This will make healthier soil and healthier crops, while also mitigating the effects of climate change, solving two problems at once. That's the basic gist of it.
Hope this answer helps you. Sorry I couldn't make it longer.
Answer:
Iron oxides appeared after the emergence of cyanobacteria.
Explanation:
The composition of Earth's atmosphere in the first couple of billions of years of its existence was nothing like the atmosphere of today. This had a big influence on the processes that were taking place, or rather what processes and to what extent could have happened in those conditions. One big difference between the atmosphere then and after is the levels of oxygen.
Until the appearance of cyanobacteria, the oxygen levels in Earth's atmosphere were very low, and the same goes for the oceans. With a lack of oxygen, the process of oxidation was absent as well. The cyanobacteria though managed to produce oxygen, and this was on such a high scale that they changed the composition of Earth's atmosphere and the oceans. Not just that this enabled complex lifeforms to develop, but it also enabled the process of oxidation. Iron oxides for example occurred only after cyanobacteria appeared, and this can easily be seen when dating the oldest iron oxides and compare that age with the appearance of cyanobacteria.
