Papers Read on Earth Sciences

Rob

Papers Read on Earth Sciences

A daily Education podcast

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Papers Read on Earth Sciences

Rob

Papers Read on Earth Sciences

Episodes
Papers Read on Earth Sciences

Rob

Papers Read on Earth Sciences

A daily Education podcast
Good podcast? Give it some love!
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Episodes of Papers Read on Earth Sciences

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Transformer-based models consist of interleaved feed-forward blocks - that capture content meaning, and relatively more expensive self-attention blocks - that capture context meaning. In this paper, we explored trade-offs and ordering of the bl
The article creates the Geothermal Adaptation-Mitigation (Geo-AdaM) conceptual frameworks that can be used in combining mitigation and adaptation in geothermal projects.2012: Pacifica F. Achieng Ogola, Brynhildur Davidsdottir, Ingvar B. Fridl
This paper explores the potential for Nordic cooperation on adaptation; specifically, for the development of a regional adaptation strategy. In particular, it addresses two questions (1) What is the current state of adaptation in the Nordic cou
The article creates the Geothermal Adaptation-Mitigation (Geo-AdaM) conceptual frameworks that can be used in combining mitigation and adaptation in geothermal projects.2012: Pacifica F. Achieng Ogola, Brynhildur Davidsdottir, Ingvar B. Fridl
The article creates the Geothermal Adaptation-Mitigation (Geo-AdaM) conceptual frameworks that can be used in combining mitigation and adaptation in geothermal projects.2012: Pacifica F. Achieng Ogola, Brynhildur Davidsdottir, Ingvar B. Fridle
Transformer-based models consist of interleaved feed-forward blocks - that capture content meaning, and relatively more expensive self-attention blocks - that capture context meaning. In this paper, we explored trade-offs and ordering of the bl
Key Points: • Scaling low carbon technologies is fundamentally different from research, development, and demonstration of those technologies • Deploying technologies at scale requires not only innovation but also transformative policy and funda
Changes in the management of crop lands between 1965 and 1990 may have led to an additional accumulation of carbonKeywords: Agriculture, carbon emissions, carbon sink, carbon storage, forestry, land-use change, soil carbon, terrestrial ecosys
For the first time during modern instrumentation, we measure uplift (with GPS and satellite data) on the peninsula, and intense earthquake activity at the same time.Key Points:• Ambient noise-based temporal seismic wave velocity variations p
Aim To map and characterize anthropogenic transformation of the terrestrial biosphere before and during the Industrial Revolution, from 1700 to 2000.https://onlinelibrary.wiley.com/doi/epdf/10.1111/j.1466-8238.2010.00540.x
Aim To map and characterize anthropogenic transformation of the terrestrial biosphere before and during the Industrial Revolution, from 1700 to 2000.https://onlinelibrary.wiley.com/doi/epdf/10.1111/j.1466-8238.2010.00540.x
Aim To map and characterize anthropogenic transformation of the terrestrial biosphere before and during the Industrial Revolution, from 1700 to 2000.https://onlinelibrary.wiley.com/doi/epdf/10.1111/j.1466-8238.2010.00540.x
South American fires and their impacts on ecosystems increase with continued emissionshttps://rmets.onlinelibrary.wiley.com/doi/epdf/10.1002/cli2.8
The hydrological characteristics of a river, including the magnitude and timing of high and low flows, are important determinants of its ecological functioning. Climate change will alter these characteristics, triggering ecological changes in r
Conditions for Achieving Sustainable Development, Eradicating Poverty and Reducing Inequalities
Sustainable Development Pathways to 1.5 C
Mitigation and Sustainable Development
Climate Adaptation and Sustainable Development
Scope and Delineations and Poverty, Equality and Equity Implications of a 1.5°C Warmer World
Integration and Enabling Transformation and Knowledge Gaps and key Uncertainties
Implementing Far-Reaching and Rapid Change
Systematic Changes for 1.5C-Consistent Pathways
Accelerating the Global Response to Climate Change and Pathways Compatible with 1.5°C: Starting Points for Strengthening Implementation
Implications of Different 1.5°C and 2°C Pathways
Avoided Impacts and Reduced Risks at 1.5°C Compared with 2°C of Global Warming
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