Answer:
Legitimate
Explanation:
One crucial indicator of a stable political system is that elections take place regularly following established procedures and that people recognize the outcomes as being Legitimate. For you to decide that a state is experiencing a stable political system, it means that their elections are timely and the result should be regarded as fair.
<u>Psychosocial intervention </u>is recommended as the first-line treatment for people affected with delirium.
<u>Explanation:</u>
Psychosocial intervention deals with the psychological problem. If a person is disconnected with the society, the psychosocial intervention performs some therapies to the person to reintegrate into society in a healthful way.
Psychosocial interventions are commonly used for solve the issues like social disorders, substance abuse cessation and prevents relapse.
Delirium is the sudden change in the brain causing mental confusion and emotional disruption. In this case, Psychosocial intervention is the recommended as the first-line treatment.
They are allowed to check the judicial branch because they are over the judicial.<span />
Because of the fluctuation.
In most ocean regions, wind-driven circulation, which has been the focus of discussions so far, does not reach below the first kilometer of the oceans. The renewal of the waters below this depth is achieved by currents that are guided by differences in density produced by effects of temperature (thermals) or salinity (halinos). The associated circulation is therefore referred to as the thermohaline circulation. Since these movements are mostly quite slow, it is very unlikely to use direct current meters (current meters); they are usually estimated by the distribution of the physical properties of the water and the application of geostrophy.
The driving force of thermohaline circulation is the formation of water bodies. Water bodies with well-defined salinity and temperature characteristics are created in specific regions by surface processes; they then sink and slowly mix with other bodies of water as they move. The two main processes for the formation of water bodies are deep convection and subduction. Both are linked to the dynamics of the mixing layer on the surface of the ocean; thus, it is necessary to first discuss thermohaline aspects of the surface ocean first.