When I am talking about land use land cover change what we have found is that if you consider last 20 years or 30 years of land use land cover data from satellite images there is a huge change in forest land to crop land there is a conversion of forest land to crop land. When you are converting forest land to crop land the deep area index or deep area density reduces or green factors reduces and when the green factor reduces the your boat transportation reduces when your boat transportation reduces the moisture supply from land surface processes reduces and that result into reduction in recycle precipitation as well as total precipitation. Secondly whenever there is a change in conversion of forest land to crop land the deep rooted land becomes shallow rooted plant region. So, what will happen when it is shallow rooted again the water extraction will reduce and because of which again the boat transportation will use and the recycle precipitation will reduce which will intern reduce the total precipitation. So, in this way basically whenever there is a then deforestation there is always a change in the recycle precipitation as well as in total precipitation. There are global studies which also said that because of deforestation there is a possibility of reduction in Indian ones who are rainfall by 18 percent and so on there was a recent study in PNS but they have not really considered the you know recent change in land use and cover the no no the added value in this work is that we have actually computed the real ski called what exactly what changes that has been taking place in land use and cover over India and what are the likely impacts of that large scale changes and what we have found is that yes the results are I mean the changes are quite significant over the dunga basin and not this Indian. I mean yes I mean we quantified the impact. So, what we did exactly we have taken help of a regional model which is known as Wanda Dissertion Forecasting Model. So, what we did we have considered 2000 to 2010 period for running the model. So, we have considered the large scale circulation pattern of this period. Now, we have used we have actually coupled community land model which is the land surface model with the Wanda Dissertion Forecasting Model. Now, in the community land model we have considered a 1980s land use land cover and 2010 land use land cover. So, with the for the same circulation model we have used 1980s land use land cover and 2010 land use land cover and we have simulated the precipitation the difference between them will actually tell you what is the change because of the change of land use land cover from 1980s to 2010 because you have kept the large scale circulation pattern sink and what we have found is that using this methodology we have actually got a decreased rainfall over over the dunga basin region and not this India. And regarding this also I would like to mention something else we have also did another study but this is not because with the change in land use land cover but what we did here on a high student Amai Patak did this study with in collaboration with Professor Prawind Kumar from University of Illinois Urbanishample. So, what we have found is that we tried to track the moisture to find out the source of the rainfall and what we have found is that during the end of the monsoon these are the two regions Ganga basin and North East India where significant amount of moisture comes from the land surface processes. So, that is a different study but this study again says that whenever there is a deportation the impacts are more prominent in Ganga basin and the North East India. So, two independent studies when they are concluding when they are when you can actually link both of them then that shows the robustness of the no results and this is what we have got from this analysis. Let us first discuss why is it because I mean why is it during the end of the monsoon? But when we are talking about recycle precipitation or any feedback that is coming from the vegetation. So, it is it is happening like this when the soil is full of moisture then vegetation can easily extract that moisture and your transcurration increases. Now, during the initial period of monsoon when it is I mean when the soil is almost in dry condition because of pre monsoon summer and so on there is not enough moisture that will lead to increase the evapotranspiration and that may significantly contribute to the moisture source of monsoon. But during after july after july after getting a good amount of rainfall the soil gets almost recharged and vegetation can easily extract the moisture and when they can easily extract the moisture the evapranspiration increases and they will you know the moisture to the you know atmospheric moisture storage and then results into good rainfall. So, the idea is during the end of the monsoon evapotranspiration is high and because of whose recycle precipitation is high and total precipitation is high. The second question is why is it so prominent in northeastern India as well as in the Ganga-Bhysin region and not really in the peninsula in India. This is because in the northern India you know the Ganga-Bhysin region as northeastern India there is a some kind of you know internal circulation that normally takes place because of Himala as another regions there is always a some kind of internal circulation. So, the moisture that is being generated from the land surface that gets I know I mean that will be always in the same region mostly and because of which the recycle component is very high. But if you are considering the peninsula in India there is a huge wind flux that is coming from there is a southwest wind flux and that is not getting constrained by any kind of specific you know geographical characteristics and because of which you know recycle component is not that high in the in the peninsula nature and because of that the impacts of dep in the peninsula nature and because of that the impacts of dep of the situation is also not that much high as compared to the northeastern India. We cannot really mention this one is higher up this one is lower and it is very difficult to say because again all of them are kind of highly correlated. Let us see if you are talking about large scale impacts let us say we are talking about western Indian ocean warming that results into decreasing the land ocean contrast of temperature and that results into moisture I mean low moisture loss. Basically when you as I was mentioning that during the initial period of months we did a huge moisture loss that is coming from the Arabian sea and Indian ocean and that results into good rainfall over Indian land mass and because of which the soil moisture gets researched and then that results into good even for transpiration and then again the cycle precipitation good recycle precipitation. Now the question is let us say if you may if you consider a bad large scale circulation pattern which is not really favorable for a good monsoon year then what will happen that will result into results into not really very good rainfall during the initial period of monsoon and that results into low discharge of soil moisture and that again results into low your transportation and low recycle precipitation. So you cannot say this one is I mean I mean this is contributing more or this is contributing less all of them are related to each other and the and the target of I mean I mean and the objective atmospheric science is to really understand all these linkages and model them in an integrated way rather than focusing just on a specific factor. So they are all integrated with each other. I mean the significance is quite important because I mean I mean whenever we are going for any kind of adaptation policies and so on we are mostly interested what will be what will be the final future projections or where interest in the climate change projection and majority of the climate models normally considered you know the increase in our emissions because of which there is interest, radiative forcing and so on but mostly the impact I mean the future land use land covered change scenarios change land use land cover scenarios and their impacts is kind of not really very much considered and secondly monsoon is you know always beginning to be a you know beginning to be a large scale phenomenon local scale effects are normally ignored in majority of the analysis on Indian monsoon but this is the first time we have mentioned that well land use land covered change that has been taken place over last 20 or 30 years that has huge impact and this should not be ignored. So even if you are going for future climate change projections don't just really want the global climate models but at the same time you just get the future land use land cover change to a regional model with the future land use land cover change land use land cover and get the future projection that will be more realistic than just considering the global climate model outputs without considering any land use land cover change.