NASA скрывает от "неавторизованной" публики собственные исследования, разоблачающие зеленую пропаганду

Вот полный текст. В ней перечислены факторы, солнечное излучение, человеческая активность, атмосфера, отражение.  И говорится что НАСА все это изучает.  Это все довольно банально, и можно найти в любом детском учебнике по природоведенью.  

What are the primary forcings of the Earth system?

The Sun is the primary forcing of Earth's climate system. Sunlight warms our world. Sunlight drives atmospheric and oceanic circulation patterns. Sunlight powers the process of photosynthesis that plants need to grow. Sunlight causes convection which carries warmth and water vapor up into the sky where clouds form and bring rain. In short, the Sun drives almost every aspect of our world's climate system and makes possible life as we know it.

Earth's orbit around and orientation toward the Sun change over spans of many thousands of years. In turn, these changing "orbital mechanics" force climate to change because they change where and how much sunlight reaches Earth. (Please see for more details.) Thus, changing Earth's exposure to sunlight forces climate to change. According to scientists' models of Earth's orbit and orientation toward the Sun indicate that our world should be just beginning to enter a new period of cooling -- perhaps the next ice age.

However, a new force for change has arisen: humans. After the industrial revolution, humans introduced increasing amounts of greenhouse gases into the atmosphere, and changed the surface of the landscape to an extent great enough to influence climate on local and global scales. By driving up carbon dioxide levels in the atmosphere (by about 30 percent), humans have increased its capacity to trap warmth near the surface.

Other important forcings of Earth's climate system include such "variables" as clouds, airborne particulate matter, and surface brightness. Each of these varying features of Earth's environment has the capacity to exceed the warming influence of greenhouse gases and cause our world to cool. For example, increased cloudiness would give more shade to the surface while reflecting more sunlight back to space. Increased airborne particles (or "aerosols") would scatter and reflect more sunlight back to space, thereby cooling the surface. Major volcanic eruptions (such as that of Mt. Pinatubo in 1992) can inject so much aerosol into the atmosphere that, as it spreads around the globe, it reduces sunlight and cause Earth to cool. Likewise, increasing the surface area of highly reflective surface types, such as ice sheets, reflects greater amounts of sunlight back to space and causes Earth to cool.

Scientists are using NASA satellites to monitor all of the aforementioned forcings of Earth's climate system to better understand how they are changing over time, and how any changes in them affect climate.

То же самое, но более подробно, написано на сайте сегодня:

Forcings: The initial drivers of climate.

Solar Irradiance. Solar radiation is the source of heat for planet Earth. Scientists also use evidence from proxy measurements, such as sunspot counts going back centuries and ancient tree rings, to measure the amount of Sun that reaches Earth’s surface. The Sun has an 11-year sunspot cycle, which causes about 0.1% of the variation in the Sun’s output.1 The solar cycle is incorporated into climate models.

Greenhouse gas emissions. Since the industrial revolution, concentrations of greenhouse gases such as carbon dioxide (CO2), methane (CH4), and nitrous oxide (N2O) have risen in the atmosphere. Burning fossil fuels such as coal, oil and gas has increased the concentration of atmospheric carbon dioxide (CO2) from 280 parts per million to 393 parts per million.2 These greenhouse gases absorb and then re-radiate heat in Earth’s atmosphere, which causes increased warming.

Aerosols, dust, smoke, and soot. Very small airborne particles come from both human and natural sources and have various effects on climate. Sulfate aerosols, which result from burning coal, biomass, and volcanic eruptions, tend to cool the Earth. Other kinds of particles such as black carbon have a warming effect.3 The global distribution of aerosols is being tracked from the ground and from satellites.

Climate feedbacks: processes that can either amplify or diminish the effects of climate forcings. A feedback that increases an initial warming is called a "positive feedback." A feedback that reduces an initial warming is a "negative feedback."

Clouds. Clouds have an enormous impact on Earth's climate, reflecting about one third of the total amount of sunlight that hits the Earth's atmosphere back into space. Even small changes in cloud amount, location and type could have large consequences. A warmer climate could cause more water to be held in the atmosphere leading to an increase in cloudiness and altering the amount of sunlight that reaches the surface of the Earth. Less heat would get absorbed, which could slow the increased warming.

Precipitation. Global climate models show that precipitation will generally increase due to the increased amount of water held in a warmer atmosphere, but not in all regions. Some regions will dry out instead. Changes in precipitation patterns, such as increased water availability, may cause an increase in plant growth, which in turn could potentially removing more carbon dioxide from the atmosphere.

Greening of the forests. Natural processes, such as tree growth, remove about half of human carbon dioxide emissions from the atmosphere every year. Scientists are currently studying where this carbon dioxide goes. The delicate balance between the absorption and release of carbon dioxide by the oceans and the world’s great forested regions is the subject of research by many scientists. There is some evidence that the ability of the oceans or forests to continue absorbing carbon dioxide may decline as the world warms, leading to faster accumulation in the atmosphere.

Ice albedo. Ice is white and very reflective, in contrast to the ocean surface, which is dark and absorbs heat faster. As the atmosphere warms and sea ice melts, the darker ocean absorbs more heat, causes more ice to melt, and makes the Earth warmer overall. The ice-albedo feedback is a very strong positive feedback.

Climate tipping points: When Earth’s climate abruptly moves between relatively stable states.

Ocean circulation. As Arctic sea ice and the Greenland ice sheet melt, ocean circulation in the Atlantic may divert the Gulf Stream. This and/or other changes would significantly change regional weather patterns. A change in the Gulf Stream could lead to a significant cooling in Western Europe. This highlights the importance of ocean circulation in maintaining regional climates.

Ice loss. Due to the strong positive feedback of the ice albedo, if enough ice melts, causing Earth’s surface to absorb more and more heat, then we may hit a point of no return. Shrinking ice sheets contribute to sea level rise. Many hundreds of millions of people live near a coast, so our ability to predict sea level rise over the next century has substantial human and economic ramifications.

Rapid release of methane. Deposits of frozen methane, a potent greenhouse gas, and carbon dioxide lie beneath permafrost in Arctic regions. About a quarter of the Northern hemisphere is covered by permafrost. As the environment warms and the permafrost thaws, these deposits can be released into the atmosphere and present a risk of runaway warming.4
 

Покажите конкретную предсказательную модель, которой вы оперируете.   Как именно выглядит математическая функция изменения температуры от человеческой деятельности.

Вы действительно думаете что климат на земле можно описать формулой?

Климатические модели это программы которые работают на суперкомпьютерах. Их можно протестировать на прошлых данных, чтобы потвердить их правильность.

ООН создало в далеком 1988 году организацию IPCC (The Intergovernmental Panel on Climate Change), в которую входят представители почти всех стран мира, включая Россию.  Они уже пять отчетов опубликовали.  Вот тут на 1552 страницах они подробно все разбирают, и приводят ссылки на сотни научных исследований.

https://www.ipcc.ch/report/ar5/wg1/