धरती का इंडिकेटर है 'थर्ड पोल', जानें क्यों जरूरी है हिमालय, ग्लोबल वार्मिंग से सीधा कनेक्शन

ETVBHARAT

'थर्ड पोल' कई देशों के वैज्ञानिकों के स्टडी ग्रुप का एक वर्चुअल प्लेटफार्म है, ये हिमालय पर क्लाइमेट चेंज को लेकर काम करता है

Transcript

00:00The third pole is made especially for crisis science.

00:04It is made for snow and glacier.

00:07We have two poles.

00:09South pole and North pole.

00:11South pole is Antarctic and North pole is Arctic.

00:15The third thing is because the maximum snow cover and glacier

00:20are in North and South pole.

00:25It is about 97% of the land market.

00:31It is about 84% in Antarctica.

00:36It is about 13.8% in the Arctic.

00:40But in the remaining 3% of the sea,

00:44the maximum mountain glacier is in Asia.

00:50In Europe, South America.

00:56Sometimes we call the Alps, the Andes, the Rockies.

01:04There are many glaciers.

01:06The maximum glacier is in Asia.

01:12It is about 3.8% in Asia.

01:19The glacier is in Asia.

01:23It is about the Manly, Karakarom area.

01:26It is about Afghanistan.

01:29India is about to come.

01:31India is about to come.

01:32India is about to come.

01:33India is about to come.

01:34India is about to come.

01:35Nepal is about to come.

01:36And Tibet is about to come.

01:38Chinese is about to come.

01:40So this is another of the Chinese glacier.

01:44There is literally a glacier in Asia.

01:45If do we have to get rid of them,

01:48the environment and like the tropography of the plane.

01:51The first of the Asia分鐘,

01:53we used to call it as a怖及ap temperature

01:55for came from March.

01:56Now, we've introduced third port.

01:57The main thing is important because

01:59three port,

02:00two port,

02:01there are four port to north port and south port.

02:05In Israel is았�ed

02:12glacier after two pools. The second thing is that this area is a continental area, which

02:21is the South Pole or North Pole, it is a whole pool. There is no more habitation. It is

02:30a snow ice glacier. The mountain area is a glacier ice, and the underground area is

02:39the irrigation land, habitation, everything. It is a whole ecosystem. The second part

02:46is that it is in such a situation where its topography and climatic conditions are very sensitive

02:53and very clear that it is a very good place to study climate. Because its extension,

03:02it is a vast area, latitude and latitude. If we look at it in the latitude, it reaches

03:0926 degrees to 36 degrees to 37 degrees. There is a huge gap in the degree. There is a lot of

03:14changes in the topography. The second part is that if you look at it climatically,

03:20we look at it from the north, east and west. If we look at it from the north,

03:26we look at it from the north. If we look at it from the north, we have two sources.

03:30One is our Indian island and the other is our Asian monsoon. This is for summer.

03:36And for winter…

03:38So the Indian island is our mountain and western distribution?

03:41Yes, western distribution is our winter, which gives maximum snowfall in the whole country.

03:47So the future impacts on western, the island has to be increased. If you come here,

03:54you come here, where you come here, when you come here, you go there, the atmosphere is

03:56no longer than you. The sun and cover is no longer.

03:58We look at it within the island, so this is a area that we look at the central island.

04:04First of all, you said that the monsoon affects this too.

04:08So the monsoon effect is more of this.

04:11The monsoon effect is more of this.

04:14Yes, the question is that the western side of the western side is coming from the winter,

04:20but if the monsoon goes from the eastern side of the western side,

04:24then the western side of the western side of the western side is more rainfall.

04:28And as you go from the western side, the rainfall is less.

04:32So, this is why the eastern side of the central part is called the monsoon acclimation glacier.

04:40In the northern northern coast, there is snowfall, after a certain height, like 5000 meters above.

04:46Because the height is more than a cool place, so there is snowfall.

04:50So, our example is the central haemalai, which is Utra Khan and Nepal.

04:58So, this is the transcendent zone.

05:01This is the transcendent zone, because it is equally the precedence.

05:07It is also the western side of the western side of the western side of the western side,

05:10and also the monsoon.

05:12So, in this year, there are some moisture activities.

05:16That's why this area is very sensitive.

05:20You might see the glacier here,

05:23the avalanche, the apada, the disturbance, the disturbance,

05:28the climatic variety is very much.

05:32So, in Himalaya, there is a signature here.

05:36There is a difference between the climate,

05:39and the whole world type of climate and land,

05:45which is the climate control.

05:47That is the signature here.

05:49So, if you want to study Himalaya,

05:52then you will get these things.

05:55So, in this way, Himalaya is very important.

05:58Many food.

05:59You can say that it is very good for the climate.

06:03Here, the acidity is very good.

06:07You have a lot of things.

06:10The longitudinal difference is very high.

06:12The longitudinal difference is very high.

06:14The longitudinal difference is very high.

06:16In the middle of the mountain,

06:18in Himalaya, you have found the average.

06:21So, in some ways, the Himalaya is very important.

06:24By the direction of the Biodivership,

06:26the Biodivership is very important.

06:28This is why Himalaya is very important.

06:31Okay.

06:32Now, what is happening?

06:34We are saying that the glacier is a faster melting.

06:36Because it is an in-beat process.

06:39accumulation, melting and accumulating is a heavy type of glacier in-build process.

06:46If it is not, it will be finished or it will be done in a long time.

06:50So, this is a single-relipping process.

06:56In winter, it will be released and in summer it will be released in the melt water fountain.

07:02So, when the glacier is created, the ice fountain is created.

07:07Now, it will be released in a few years.

07:12But in the last few years, the last little ice age,

07:17which is in 1850-1850,

07:22the glacier has been extended and increased the volume.

07:30But after the little ice age, the continuous glacier has been treated.

07:36So, the first thing happened, we didn't have much attention to it.

07:41There was a lot of attention.

07:43But in a few days, we felt that the glacier is being reduced,

07:46the glacier is being treated.

07:48So, we thought that the climate has changed.

07:51The temperature has increased, the earth's increased.

07:54So, this is what we started to do.

07:57I think that the 70s, we still don't consider the climate.

08:01We still don't consider the climate.

08:02In the 70s, 80s.

08:03We still don't consider the glacier.

08:04The glacier is being treated.

08:05In that way, the environment is being treated.

08:07In that way, the environment is being treated.

08:08Or the mountain environment.

08:09So, it is a power of the temperature.

08:10It is a power of the temperature.

08:13But when we saw that this is a significant process,

08:17which is a growing process,

08:20which is a growing process,

08:22which is a very fragile impact,

08:24which is a very sensitive temperature,

08:26which is a very sensitive effect.

08:28So, the climate change and global warming.

08:40There are two different things.

08:42In the climate change,

08:44there are all the factors of the climate change.

08:46The climate change, there are seasonal changes.

08:49And there is an annual,

08:52which is a whole system in the earth's rotting.

08:56What is global warming?

08:58Global warming is only one parameter.

08:59The temperature.

09:01The climate change.

09:02The climate change.

09:03We just spoke about global warming,

09:06because the temperature of the climate change,

09:08the climate change.

09:09The climate change,

09:10and the atmosphere of the climate change.

09:12So, this is global warming.

09:14In this global warming,

09:16the temperature is one parameter.

09:18It is a simple temperature,

09:20In which the other parameters of the weather, it distracts itself.

09:27Whether it is albedo, whether it is humidity, whether it is radiation, whether it is precipitation.

09:37There is a lot of pressure on your prism.

09:39If I can see it, there is a lot of effect on the prism.

09:43The prism means the rain and snow.

09:49So there is a lot of change in the rain.

09:51The rain has increased.

09:54The snow cover area is reduced.

09:57The snow cover area is reduced.

09:59We talked about the rain before.

10:01The rain was very low.

10:07The snow falls.

10:10But the rain has reached until 4000-5000.

10:13So that is an indicator of the temperature of the climate.

10:16The glow of the rain is mainly anthropogenic.

10:23Carbon emissions.

10:24We use fuel, pollution, pollution and pollution.

10:28What is the waterfront?

10:30The waterfront is reduced.

10:33The waterfront is increased.

10:35The gas well producing temperature of the waterfront, it has increased.

10:41Our rain is socially그 temperature.

10:43His temperature is increased.

10:44These two things that I quanBO show.

10:46The temperature followed by you is that...

10:49Your winter is increased.

10:50The winter pluses covered.

10:54The winter pluses aumento.

10:55The warm clock is increased.

10:59In the first October, the glacier falls, and the winter period has been sinking.

11:06Now, the snow falls starts in March or February, and it's less than a day.

11:13But the warm time has increased, and the warm time has decreased.

11:19So, the glacier has increased.

11:22The glacier is in its own place.

11:24After all, the snow is fully balanced.

11:30It's only dark, but only 200 to 350 meters, and they can have it.

11:32The Icelandic acid will not be delayed.

11:36The winter period has decreased, but the winter period has increased.

11:40When you die through the weather, the heat is increased.

11:44The waves have increased, the time period has increased.

11:50The time period has increased.

11:52In October the meeting, you will have contact with the normal.

11:56And the size of the glacier is reduced, the speed is increased.

12:02You can tell us that if you have a large ice cube,

12:06you will have a small ice cube.

12:08You will have a large ice cube, you will have a large ice cube,

12:12but if you have a small size, you will have a speed.

12:16That's right.

12:18What is happening in Himalaya?

12:20What is happening in Himalaya?

12:22If we talk about Himalaya or some of the whole earth,

12:26because the glaciers are different.

12:30The small glaciers, the big glaciers,

12:32the big glaciers, the big glaciers,

12:34the continental glaciers, the big glaciers,

12:37the polar glaciers in Antarctica,

12:40the high seats are very big.

12:42The thickness is 400-500 meters.

12:46So, our glaciers, the mountain glaciers,

12:50they are about 200-500 meters.

12:52The length is about 30-50-100 kilometers.

12:56But what is happening?

12:58We have less of them.

13:00If I look at Himalaya,

13:02in Himalaya,

13:04in Himalaya,

13:06the latest inventory,

13:08which we see in Himalaya,

13:10it is about 9,500 glacier.

13:12Right from Jambukasmi to Aranthar Parjish,

13:14Indian part.

13:16Indian Himalaya.

13:18In the 1950s,

13:19there are 600-600% of the small glaciers,

13:22whose size is 1-100 km.

13:24They are from Delhi.

13:26That's why we have an alarming glacier.

13:28But the big glaciers,

13:30say, 5 square kilometers,

13:32from 5 square kilometers,

13:34we have 30% of the glacier.

13:36It is less.

13:38But its volume is very much.

13:40And its volume is very low.

13:42So, if the sankhya is low,

13:46the number is no matter.

13:50Okay?

13:52Size is matter.

13:54What we say about Global Rhyme,

13:56Global Rhyme is an anthropogenic activity.

13:58Anthropogenic activity,

14:00which we are born from Manoj.

14:02Human made.

14:04So, what is your pollution?

14:06Your pollution is very high.

14:08Your carbon emission is very high.

14:12Air agriculture has a very high effect.

14:14Biodiversity has a very high effect.

14:16So, it will increase.

14:18Because this is a subject

14:20that you have a lot of work.

14:22The climate change,

14:24the IPCC is very good.

14:26So, I have the idea

14:28that carbon emission will reduce

14:30carbon emissions.

14:32it is a very low carbon emission.

14:34If there is a lot of work,

14:36we are being able to reduce the amount of fuel.

14:38We are getting less than the fuel.

14:40As we say,

14:42the fuel is one of the electric,

14:44we are getting less than the fuel.

14:46In the fuel,

14:48we are getting less.

14:49We are getting less than the methane.

14:51Now, what is this in the trees?

14:53What is the glycery?

14:55There is a tree we are getting from the fire.

14:57There is a farm that we are getting from the fire.

14:59which is ice, but in the rain, the soil is dry.

15:03But in the warm water, the water will be released.

15:08Sometimes the water will be converted into the room.

15:12So, the methane is released a lot.

15:14That's also the glacier?

15:15Yes, that's also the glacier.

15:17So, these things are the same.

15:20When we talk about climate change,

15:24we talk about current emissions and pollution.

15:28So, how do we reduce it?

15:31We focus on what we do.

15:33How do we reduce the plastic?

15:34How do we reduce the plastic role?

15:37No, plastic is a big role.

15:39I always work with the glacier.

15:42I go to the glacier every year.

15:45Every year, at least 8-10 years,

15:48I use the water to lower the glacier.

15:50Like the tinker-dub, plastic, this.

15:53People go there and throw it.

15:55When we go to the glacier, we go to the glacier.

16:00We go there and throw it.

16:01Direct impact?

16:02Direct impact.

16:03What is that?

16:04Because it doesn't decompose.

16:06Okay.

16:07Now, if you do what you do,

16:09you do the glacier,

16:10then the glacier will raise the elevator.

16:12It will raise the radiation.

16:13It will be more exposed.

16:14It will be disturbed.

16:16These things become great.

16:20So, if we do small things, we will start with a good relationship.

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