Uncertainties in Prediction of Future Sea Level Rise Due to Impact of Climate Change

On reviewing the development of the research methodologies on climatechangeandsealevelriseduringthe lasttwodecades, it is observed that the assumed scenarios for apprehending the rise in global temperature are groundedona lotofuncertainties.Thereal-timedatavaries from IPCC’s predictions. The gradual...

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Main Author: SUDIPTA CHAKRABORTY
Format: Article in Journal/Newspaper
Language:unknown
Published: Kudos Innovations Ltd 2021
Subjects:
Online Access:https://dx.doi.org/10.26303/ga5f-m008
https://link.growkudos.com/1pry79lcrnk
id ftdatacite:10.26303/ga5f-m008
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spelling ftdatacite:10.26303/ga5f-m008 2023-05-15T16:41:18+02:00 Uncertainties in Prediction of Future Sea Level Rise Due to Impact of Climate Change SUDIPTA CHAKRABORTY 2021 https://dx.doi.org/10.26303/ga5f-m008 https://link.growkudos.com/1pry79lcrnk unknown Kudos Innovations Ltd Collection article Webpage 2021 ftdatacite https://doi.org/10.26303/ga5f-m008 2021-11-05T12:55:41Z On reviewing the development of the research methodologies on climatechangeandsealevelriseduringthe lasttwodecades, it is observed that the assumed scenarios for apprehending the rise in global temperature are groundedona lotofuncertainties.Thereal-timedatavaries from IPCC’s predictions. The gradual transition on the emission pathway scenarios from SRES (2000) till RCPs in AR5 of IPCC depicts the conceptual difference between the two concepts in scenarios. SRES represented detailed socio-economic-based scenarios, but RCPs are based on the capacity of a gas affecting the change in energy in the atmosphere due to GHG emissions known as Radiative Forcing. Considering the possible range of theradiative forcing values in 2100, AR5 of IPCC considers the four RCPs numbered as 2.6,4.5, 6.0 and 8.5 as per greenhouse gas concentration trajectories (not emissions). The present condition of meltingofice sheetsatAntarcticaandGreenlandisquite high and it is understood that such melting will continue. Even in a situation, if the anthropogenic emission of GHGs is immediately stopped, the self-sustained melting will continue. Models so far being based onnumerical and probabilistic approaches are expected to undergo abrupt change because of the current inconsistent ice sheet dynamics. Considering deep uncertainty in socio-political and economic changes amongst nations, the importance of usability of model hierarchy for the complex science of climate change is becoming unforecastable, in the prevalent ice dynamics during accelerated warming situations. In reality, the predictions are becoming less reliable. Possibility of the scenarios likely to be changed are apprehended during the advent of CMIP6 and the variations in contributing factors in the form of SSPs in the upcoming IPCC AR6, in2022 and it is indicated that the research may take a new turn. A multidisciplinary approach to research with minimum uncertainty ina more precise and finer manneris the need of the day Article in Journal/Newspaper Ice Sheet DataCite Metadata Store (German National Library of Science and Technology)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language unknown
description On reviewing the development of the research methodologies on climatechangeandsealevelriseduringthe lasttwodecades, it is observed that the assumed scenarios for apprehending the rise in global temperature are groundedona lotofuncertainties.Thereal-timedatavaries from IPCC’s predictions. The gradual transition on the emission pathway scenarios from SRES (2000) till RCPs in AR5 of IPCC depicts the conceptual difference between the two concepts in scenarios. SRES represented detailed socio-economic-based scenarios, but RCPs are based on the capacity of a gas affecting the change in energy in the atmosphere due to GHG emissions known as Radiative Forcing. Considering the possible range of theradiative forcing values in 2100, AR5 of IPCC considers the four RCPs numbered as 2.6,4.5, 6.0 and 8.5 as per greenhouse gas concentration trajectories (not emissions). The present condition of meltingofice sheetsatAntarcticaandGreenlandisquite high and it is understood that such melting will continue. Even in a situation, if the anthropogenic emission of GHGs is immediately stopped, the self-sustained melting will continue. Models so far being based onnumerical and probabilistic approaches are expected to undergo abrupt change because of the current inconsistent ice sheet dynamics. Considering deep uncertainty in socio-political and economic changes amongst nations, the importance of usability of model hierarchy for the complex science of climate change is becoming unforecastable, in the prevalent ice dynamics during accelerated warming situations. In reality, the predictions are becoming less reliable. Possibility of the scenarios likely to be changed are apprehended during the advent of CMIP6 and the variations in contributing factors in the form of SSPs in the upcoming IPCC AR6, in2022 and it is indicated that the research may take a new turn. A multidisciplinary approach to research with minimum uncertainty ina more precise and finer manneris the need of the day
format Article in Journal/Newspaper
author SUDIPTA CHAKRABORTY
spellingShingle SUDIPTA CHAKRABORTY
Uncertainties in Prediction of Future Sea Level Rise Due to Impact of Climate Change
author_facet SUDIPTA CHAKRABORTY
author_sort SUDIPTA CHAKRABORTY
title Uncertainties in Prediction of Future Sea Level Rise Due to Impact of Climate Change
title_short Uncertainties in Prediction of Future Sea Level Rise Due to Impact of Climate Change
title_full Uncertainties in Prediction of Future Sea Level Rise Due to Impact of Climate Change
title_fullStr Uncertainties in Prediction of Future Sea Level Rise Due to Impact of Climate Change
title_full_unstemmed Uncertainties in Prediction of Future Sea Level Rise Due to Impact of Climate Change
title_sort uncertainties in prediction of future sea level rise due to impact of climate change
publisher Kudos Innovations Ltd
publishDate 2021
url https://dx.doi.org/10.26303/ga5f-m008
https://link.growkudos.com/1pry79lcrnk
genre Ice Sheet
genre_facet Ice Sheet
op_doi https://doi.org/10.26303/ga5f-m008
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