The following is a summary and article by AI based on a transcript of the video "Climate Science, Risk and Solutions: The MIT Climate Primer". Due to the limitations of AI, please be careful to distinguish the correctness of the content.
00:00 | [Music] |
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00:06 | we know that you know that the Earth is |
00:09 | warming but you might have questions |
00:11 | like how did scientists figure out that |
00:13 | this warming is happening and that it's |
00:15 | caused by humans how strong is the |
00:17 | evidence really what risks can we expect |
00:20 | and what can we do about them climate |
00:22 | science is not a new field by the time |
00:25 | of the American Civil War scientists |
00:27 | understood that the Earth is kept warm |
00:29 | by a a handful of gases that make up |
00:31 | less than 1% of our atmosphere but that |
00:34 | these gases keep the sun's radiation |
00:37 | from being immediately lost to outer |
00:39 | space and they understood that if humans |
00:42 | were to change the amount of these gases |
00:44 | in our atmosphere our climate would be |
00:47 | transformed today these predictions are |
00:50 | coming to life and as global |
00:51 | temperatures rise and extreme weather |
00:54 | intensifies you probably have more |
00:56 | questions the online primer climate |
00:59 | science R and solutions from the |
01:01 | Massachusetts Institute of Technology is |
01:03 | our effort to bring the story of climate |
01:06 | science to everyone who wants to learn |
01:08 | used in universities and high schools |
01:11 | around the world this primer answers how |
01:14 | scientists know what they know about |
01:16 | climate change it takes Learners through |
01:19 | the history of climate science the risks |
01:21 | we face now and will face in the future |
01:24 | and the options we have to overcome |
01:26 | climate change and secure a safe and |
01:29 | prosperous planet for ourselves and for |
01:31 | future generations to do this we worked |
01:34 | with mit's Professor Carrie Emanuel an |
01:36 | acclaimed climate Communicator who has |
01:38 | been studying the Earth's weather system |
01:40 | for over 40 years so let's let him share |
01:43 | a peek at what you'll learn in climate |
01:45 | science risk and solutions from MIT |
01:49 | human cause climate change began with |
01:51 | the Industrial Revolution when people |
01:54 | began burning large quantities of coal |
01:56 | and oil releasing carbon dioxide into |
01:58 | the atmosphere and although scientists |
02:00 | have long predicted that this influx of |
02:03 | CO2 would raise the Earth's temperature |
02:05 | now that we can see it happening a very |
02:07 | reasonable question people ask is how |
02:10 | can we Trace these Trends all the way |
02:12 | back to the dawn of the fossil fuel age |
02:15 | surely that's too long ago for us to |
02:16 | have accurate records of world |
02:18 | temperatures let alone how much carbon |
02:20 | dioxide was in the air in fact by the |
02:23 | 19th century people were using |
02:25 | thermometers and keeping careful records |
02:27 | of temperature in enough places around |
02:30 | the globe for us to reconstruct average |
02:32 | World temperatures naturally most of |
02:35 | these measurements were taken at |
02:36 | landbased stations but some came from |
02:38 | the ocean surface too this is crucial |
02:41 | data when trying to learn the Earth's |
02:43 | average surface temperature since of |
02:44 | course the oceans take up most of the |
02:46 | world's surface it's not enough to |
02:48 | Simply average all the temperature |
02:50 | records we have together one must |
02:52 | carefully account for the uneven |
02:54 | distribution of temperature measurements |
02:56 | around the world the way growing cities |
02:58 | have become warmer than the surrounding |
03:00 | Countryside and many other variables but |
03:03 | one way to know if our calculations are |
03:05 | good is to see if different groups |
03:07 | working independently of each other have |
03:09 | reached the same conclusions and indeed |
03:12 | the five major groups tracking global |
03:14 | temperatures have produced very similar |
03:16 | records discovering the same ups and |
03:18 | downs from year to year since the 1960s |
03:21 | we have been able to add satellite |
03:23 | measurements of infrared radiation at |
03:26 | the Earth's surface to our arsenal of |
03:28 | instruments and it is reassuring to see |
03:30 | that these two track closely with the |
03:32 | thermometer record from around the world |
03:35 | what about carbon dioxide how can we |
03:37 | really know the temperature rise traced |
03:39 | by all these different sources is caused |
03:41 | by Rising CO2 levels indeed it was not |
03:44 | until the 1950s that scientists began |
03:46 | measuring the CO2 content of the |
03:48 | atmosphere directly for climate |
03:50 | scientists it's not enough to know that |
03:53 | CO2 levels have been rising since the |
03:55 | 1950s we want to return to the beginning |
03:57 | of the Industrial Revolution and our |
03:59 | greatest asset here is ice taken from |
04:02 | Greenland and Antarctica as snow falls |
04:05 | in these frigid parts of the world it |
04:07 | traps small samples of air along with it |
04:10 | because the snow never melts over time |
04:12 | it becomes compressed in layers of ice |
04:15 | with tiny bubbles inside that preserve |
04:17 | ancient air this record of air samples |
04:20 | goes back hundreds of thousands of years |
04:22 | by drilling into the ice and collecting |
04:25 | cores scientists can create a |
04:27 | year-by-year record of our past |
04:29 | atmosphere and it is these ice core |
04:31 | samples that show us the history of CO2 |
04:33 | in the atmosphere which we now know held |
04:36 | steady at around 280 parts per million |
04:38 | for almost all of recorded human history |
04:41 | and tell began to creep up in the 19th |
04:44 | century and truly take off in the mid |
04:46 | 20th to the point that the CO2 content |
04:48 | of the atmosphere is fully 50% higher |
04:51 | than it was 150 years ago from these |
04:53 | combined records we can now see plainly |
04:56 | what climate scientists have predicted |
04:58 | all along Co two levels have been rising |
05:01 | as we burn fossil fuels and temperatures |
05:03 | have been rising with them the pace of |
05:06 | climate science has never been faster |
05:08 | which is why mit's climate science risk |
05:11 | and solutions has been newly updated for |
05:13 | 2024 with the latest data and scientific |
05:16 | consensus and with help from MIT open |
05:19 | learning all this information has been |
05:21 | paired with fun online learning |
05:23 | techniques where you can watch listen to |
05:25 | and play with the data all of this is |
05:27 | connected to other learning resources |
05:29 | from from MIT that will help you drill |
05:31 | deeper into the topics that interest you |
05:34 | the most whether that's the basic |
05:35 | science of the greenhouse effect the |
05:37 | climate models that help scientists peer |
05:40 | into our future climate or the solutions |
05:42 | at hand from renewable energy to carbon |
05:45 | capture are you ready to have your |
05:46 | questions answered about climate change |
05:48 | and climate science then visit climate |
05:50 | primer. mit.edu to begin |