Water Exchange Between the Gulf of Ob and the Kara Sea During Ice-Free Seasons: The Roles of River Discharge and Wind Forcing

Alexander Osadchiev,Olga Konovalova,Alexandra Gordey

doi:10.3389/fmars.2021.741143

Abstract

The Gulf of Ob is among the largest estuaries in the World Ocean in terms of area, watershed basin, and freshwater discharge. In this work, we describe the roles of river discharge and wind forcing on the water exchange between the Gulf of Ob and the Kara Sea during ice-free seasons. This work is based on the extensive in situ measurements performed during 10 oceanographic surveys in 2007–2019. Due to large river runoff (∼530 km3 annually) and low tidal forcing (&lt;0.5 m/s), the estuarine processes in the Gulf of Ob during the ice-free season are generally governed by gravitational circulation. Local wind forcing significantly affects general estuarine circulation and mixing only in rare cases of strong winds (∼10 m/s). On the other hand, remote wind forcing over the central part of the Kara Sea regularly intensifies estuarine—sea water exchange. Eastern winds in the central part of the Kara Sea induce upwelling in the area adjacent to the Gulf of Ob, which increases the barotropic pressure gradient between the gulf and the open sea. As a result, intense and distant (120–170 km) inflows of saline water to the gulf occur as compared to the average conditions (50–70 km). Remote wind forcing has a far stronger impact on saltwater intrusion into the Gulf of Ob than the highly variable river discharge rate. In particular, saltwater reaches the shallow central part of the gulf only during upwelling-induced intense inflows. In the other periods (even under low discharge conditions), fresh river water occupies this area from surface to bottom. The upwelling-induced intense inflows occur on average during a quarter of days (July to October) when the gulf is free of ice. They substantially increase the productivity of phytoplankton communities in the gulf and modify the taxa ratio toward the increase of brackish water species and the decrease of freshwater species.

Highlights

The Gulf of Ob is located in the southern part of the Kara Sea and is among the largest river estuaries in the World Ocean (Figure 1)
We focus on in situ measurements performed in the Gulf of Ob in August 2019, which revealed the most intense and distant inflow of saline seawater into the gulf, and demonstrate that these intense inflows of saline water to the gulf significantly affect qualitative and quantitative characteristics of the local phytoplankton communities
We address the water exchange between the Gulf of Ob and the open part of the Kara Sea during ice-free periods

Summary

Introduction

The Gulf of Ob is located in the southern part of the Kara Sea and is among the largest river estuaries in the World Ocean (Figure 1). Water Exchange in the Gulf of Ob from the Taz River, the Pur River, and smaller rivers (Gordeev et al, 1996; Pavlov et al, 1996). This large freshwater volume accounts for ∼15% of the total freshwater runoff to the Arctic Ocean (Guay et al, 2001) and ∼1.5% of the total freshwater runoff to the World Ocean (Oki and Kanae, 2006). Maximal discharge to the gulf is registered at the end of May and is induced by ice melting in the watershed area of the gulf (Figure 1C). Discharge during the secondary rain-induced peak can be the same or higher in the beginning of September than in May (Osadchiev et al, 2021a)

Results

Discussion

Conclusion