an algebraic variety
If a single polynomial equation cuts out a curve in the plane, what do you get from several equations in many variables at once? An algebraic variety is the answer: it is the set of points in space (of any number of dimensions) that satisfy a whole system of polynomial equations simultaneously. A line, a circle, a sphere (x^2 + y^2 + z^2 = 1), the surface where two equations both hold — each is a variety. It is the higher-dimensional, many-equation generalization of the algebraic curve, and it is the central object of algebraic geometry.
Concretely, pick polynomials f_1, f_2, ..., f_k in variables x_1, ..., x_n. The variety they define is every point (x_1, ..., x_n) for which f_1 = 0 AND f_2 = 0 AND ... AND f_k = 0 — the common zero set, the intersection of each equation's solution set. One equation in 3D typically gives a surface (a 2-dimensional variety); add a second independent equation and the solutions usually drop to a curve (1-dimensional); a third can pin it down to isolated points (dimension 0). So the DIMENSION of a variety is, roughly, the number of free coordinates left after the equations have done their constraining. As with curves, a variety is IRREDUCIBLE if it is not the union of two smaller varieties, and the irreducible ones are the genuine building blocks.
Varieties are where geometry and algebra fuse: every geometric question (Do these shapes meet? How? With what multiplicity?) becomes an algebra question about the polynomials, and vice versa — a dictionary made precise in the twentieth century by ideals, rings, and eventually schemes. This powers everything from robotics motion-planning (the configurations of a robot arm form a variety) to physics and coding theory. One honest subtlety: 'variety' is used slightly differently by different authors — some demand irreducibility, some work only over the complex numbers, some allow the more general 'scheme'. The shared core, though, is always the same: solutions of polynomial systems, viewed geometrically.
In 3D, the single equation x^2 + y^2 + z^2 = 1 is the unit sphere, a 2-dimensional variety. Now intersect it with the plane z = 0 (add the equation z = 0): the two equations together force x^2 + y^2 = 1 with z = 0 — the equator, a 1-dimensional variety. Each new independent equation typically removes one dimension, exactly the way each constraint removes one degree of freedom.
Adding an equation intersects, and intersection usually drops the dimension by one.
More equations do not always mean lower dimension. Three equations might describe the same surface a single equation does (if two are redundant), or might be inconsistent and describe nothing; dimension is governed by independence, not the raw count of equations.