NOC-MSM / Regional-NEMO-Medusa

Developing NEMO-MEDUSA in regional (anything non-global) applications
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River forcing : data #6

Open jasontempestholt opened 3 years ago

vleguenn commented 2 years ago

I. River forcing : data

Summary : It explains what river forcing data can be used for the regional NEMO-MEDUSA configuration (1/12°).

I can use two types of datasets :

-> (a) Datasets from literature -> (b) Datasets from Andrew Yool (N006 runoff file available on JASMIN) -> (c) Datasets from JRA55

a) Using datasets from literature

The table below regroups the references used to obtain seasonal river discharge.

Rivers References Period Mean annual discharge (m3/s)
Tana (Kenya) Bouillon et al. (2007) (Garissa Station) 1982 - 1996 172.34
Galana (Kenya) Marwick et al. (2014) 1959 - 1977 64.24
Pangani (Tanzania) GRDC (Korogowe Station,110 km above the mouth) 1959-1977 27.7
Wami (Tanzania) Forestry and Beekeeping Division, 2005 (Mandera Station, 50 km above the mouth) 1954-1984 60.6
Rufiji (Tanzania) GRDC (Stiegler Station, 150 above the mouth) 1954 - 1978 791.85
Ruvuma (Mozambique) Minihane (2012) (Composite Runoff) ? 1831.725

The seasonal river discharge of each rivers are shown in the figure below:

Rivers

The figure below regroups all the rivers discharge (m3 s-1) in one plot :

All_seasonal_cycle_Rivers_together_m3_s

The river discharge (m3 s-1) datasets can be obtained here (called RIVERS_FLOW): https://github.com/vleguenn/EAFRICA_R12/blob/main/RIVER/LITERATURE/RIVERS_FLOW.mat

References list :

Bouillon, S., Dehairs, F., Schiettecatte, L. S., & Borges, A. V. (2007). Biogeochemistry of the Tana estuary and delta (northern Kenya). Limnology and Oceanography, 52(1), 46-59.

Forestry and Beekeeping Division (2005) Forest condition assessment of the Eastern Arc Mountains Forests of Tanzania. Conservation and Management of the Eastern Arc Mountain Forests, Forestry and Beekeeping Division, Dar es Salaam.

Marwick, T. R., Tamooh, F., Ogwoka, B., Teodoru, C., Borges, A. V., Darchambeau, F., & Bouillon, S. (2014). Dynamic seasonal nitrogen cycling in response to anthropogenic N loading in a tropical catchment, Athi–Galana–Sabaki River, Kenya. Biogeosciences, 11(2), 443-460.

Minihane, M. R. (2012). Evaluation of streamflow estimates for the Rovuma River. Physics and Chemistry of the Earth, Parts A/B/C, 50, 14-23.

Map of the bathymetry (m) and the rivers mouth:

Bathymetry_1_12_resolution_and_river_mouths

See section I.a) (https://github.com/NOC-MSM/Regional-NEMO-Medusa/issues/9) For the results of the runs that used the above datasets for the rivers (seasonal climatology).

vleguenn commented 2 years ago

I. River forcing : data

b) Datasets from Andrew Coward (N006 runoff file available on JASMIN)

The datasets provided by Andrew Coward uses monthly runoff/river climatologies which were probably not so different to what I already have (I.a). For example, the N006 runoff file is available on JASMIN:

_/gws/nopw/j04/nemo_vol1/ORCA0083-N006/forcing/runoff_coast1pt_ant3pt_isl20_obtaz_1m_ORCA12_correctAMZ_200610_lbclnk.nc_

based originally on the Dai and Trenberth study as documented in Dai and Trenberth, 2002. The original data are available on the web : http ://www.cgd.ucar.edu/cas/catalog/dai/

For the regional configuration, I cut the runoff file to the domain of the EAFRICA model :

ncks -d x,3906,3962 -d y,1355,1478 ./runoff_coast1pt_ant3pt_isl20_obtaz_1m_ORCA12_correctAMZ_200610_lbclnk.nc -O cropped_runoff_ACow.nc

The data is available here : https://github.com/vleguenn/EAFRICA_R12/blob/main/RIVER/ANDREW_COWARD/cropped_runoff_ACow.nc

DrYool commented 2 years ago

If the correct diagnostics are available (and they might not be), it might be helpful to see what the freshwater inputs via runoff look like between the models (i.e. run 6, run 9 and N06). That might help us understand why they produce different results.

(@vleguenn - I appreciate you're against the clock here, so ignore this request if you've other things to do first.)