PHC_16 run

This run is based on the PHC_15 one except that the precipitation & runoff have been reduce by 9% instead of 8% in PHC_15.
The idea here is to minimize the SSH drift and the Empold values. The result is positive.

Comparisons (when done) are done relatively to the PHC_10 experiment to emphaze the impact of using the Kz tides parameterization especially on the ITF area.

Runs	PHC_10	PHC_11	PHC_15	PHC_16
Precip	-8%	-8%	-8%	-9%
Evap	+10%	+10%	+10%	+10%
Empold (Sv)	+0.1	+0.12	+0.13	-0.02
SST/rt PHC3	??	??	??	??
SSH drift (m)	+0.008	+0.01	+0.01	-0.002

SST differences with Reynolds and PHC_10:

---

Temperature differences at z=105 m with Levitus and PHC_10:

---

SSS differences with Levitus and PHC_10:

---

Temperature differences in zonal average with Levitus and PHC_10:

---

Salinity differences in zonal average with Levitus and PHC_10:

---

Equatorial differences with Levitus and PHC_10 of zonal velocity U:

---

Equatorial differences with Levitus and PHC_10 of temperature:

---

Equatorial differences with Levitus and PHC_10 of salinity:

---

Pacific equatorial differences with Levitus and PHC_10 of temperature:

---

Qnet differences with PHC_10 :

---

Global MOC:

---

Atlantic MOC:

---

BSF:

---

Mediterranean water Lat: 40°N, depth 700 m:

---

Mediterranean water Lat: 38°N, depth 1000 m:

Erp & Mxl fields:

Straits transport: