airDensity_30m_daily: Data: Air density (30m, daily)
In glacierSMBM: Glacier Surface Mass Balance Model
Description
Usage
Format
Details
Source
References
Examples
Description
Distributed air density at the Liligo Glacier (Karakoram, Pakistan)
Usage
1
Format
An object of class 'RasterLayer'.
Details
Dataset: The High Asia Refined Analysis (TU Berlin, Chair of Climatology)
Date: 2011-08-15
Temporal resolution: daily
Pixel resolution: 10 km
Unit: kg m-3
Projection: UTM 43 N
Note: The original dataset was resampled to a spatial resolution of 30 m using the function resample.
Source
References
Groos, A.R., Mayer, C., Smiraglia, C., Diolaiuti, G., and Lambrecht A. (submitted). A first attempt to model region-wide glacier surface mass balances in the Karakoram: findings and future challenges. Geografia Fisica e Dinamica Quaternaria.
Maussion, F., Scherer, D., Moelg, T., Collier, E., Curio, J., and Finkelnburg, R. (2014). Precipitation Seasonality and Variability over the Tibetan Plateau as Resolved by the High Asia Reanalysis. Journal of Climate 27, 1910-1927.
Examples
1
2
glacierSMBM documentation built on May 2, 2019, 3:42 a.m.
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Description Usage Format Details Source References Examples
Description
Distributed air density at the Liligo Glacier (Karakoram, Pakistan)
Usage
1 |
Format
An object of class 'RasterLayer'.
Details
Dataset: The High Asia Refined Analysis (TU Berlin, Chair of Climatology)
Date: 2011-08-15
Temporal resolution: daily
Pixel resolution: 10 km
Unit: kg m-3
Projection: UTM 43 N
Note: The original dataset was resampled to a spatial resolution of 30 m using the function resample.
Source
References
Groos, A.R., Mayer, C., Smiraglia, C., Diolaiuti, G., and Lambrecht A. (submitted). A first attempt to model region-wide glacier surface mass balances in the Karakoram: findings and future challenges. Geografia Fisica e Dinamica Quaternaria.
Maussion, F., Scherer, D., Moelg, T., Collier, E., Curio, J., and Finkelnburg, R. (2014). Precipitation Seasonality and Variability over the Tibetan Plateau as Resolved by the High Asia Reanalysis. Journal of Climate 27, 1910-1927.
Examples
1 2 |
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