Skip to content

NASA-GISS/freshwater-forcing-workshop

Repository files navigation

Table of contents

Ice Sheet Freshwater Forcing

Introduction

This repository contains discussions and workbooks (code) from a virtual workshop on Anomalous Freshwater Fluxes.

Included in this repository are:

  • GitHub Discussions from before, during, and after the workshop.
  • Workbooks (code) used to build data products (e.g. Greenlandic and Antarctic freshwater from surface melt, ice shelf melt, basal melt, icebergs, etc.).
  • Examples of data product post-processing to aid modelers who want use the data.

Workshop

The virtual workshop on Anomalous Freshwater Fluxes aimed to capture freshwater fluxes from ice sheets and ice shelves for use in climate models that don’t include interactive ice sheets. The workshop slides, videos, and discussion notes are archived at https://zenodo.org/doi/10.5281/zenodo.11127902.

To stay up-to-date with existing and new discussions, click on the watch button near the top of this page and then select All Activity or Custom > Discussions (and Issues). If you’re new to GitHub, it can be used as a collaborative project management tool (in addition to a code repository). See Braga (2023) http://doi.org/10.1111/2041-210x.14108.

Data Products

Antarctic

Iceberg Days

This data product is not meltwater from icebergs, but instead days and locations where icebergs are observed. The raw data comes from Budge (2018) http://doi.org/10.1109/jstars.2017.2784186 and is then binned in (lon,lat) bins where the values shows the number of days icebergs spend in each in. 18 maps are generated, one per Rignot (IMBIE) basin, where icebergs are assigned to the basin nearest their first recorded location.

Iceberg melt

Ice shelf melt

Surface runoff

Basal (grounded) runoff

Greenland

Surface runoff

This data product is MAR runoff distributed by Rignot (IMBIE) region, but processed at stream level by Mankoff (2020) http://doi.org/10.5194/essd-12-2811-2020. The data includes ‘ice runoff’ which comes from melted ice, snow, and rain on the ice sheet, and ‘land runoff’ which comes from melted snow and rain on land. Runoff is routed through individual streams (subglacial for ice, sub-aerial for land). Both ice-sourced and land-sourced runoff can enter the ocean either at the surface (from a terrestrial stream) or at depth subglacially. This value is estimated per stream. When summing by ROI, the minimum submarine discharge depth is provided for each ROI.

Basal runoff

See Karlsson (2023) http://doi.org/10.34194/geusb.v53.8338

Glacier termini

This product is generated from flux gates ~5 km upstream of the terminus.

It lacks:

  • Terminus retreat, which should add ~10 % over the last two decades
  • Splitting output between icebergs and submarine melt, which is ~50 % +- 40 %
  • Workbook: ./greenland_discharge.org
  • Data product: GL_discharge.nc
Solid ice calving

To do

Submarine melt

To do

About

Discussions related to a virtual workshop focusing on Greenlandic and Antarctica freshwater.

Topics

Resources

Stars

Watchers

Forks

Contributors 4

  •  
  •  
  •  
  •