Why Does Body Temperature Increase During Fever?

Your body temperature rises during a fever because your brain deliberately raises its internal thermostat. A region called the hypothalamus, which normally keeps your core temperature around 98.6°F (37°C), resets to a higher target, sometimes 100.4°F (38°C) or above. Once that new set point is established, your body treats its current normal temperature as “too cold” and activates the same warming mechanisms it would use on a freezing winter day.

How Your Brain Resets Its Thermostat

The hypothalamus acts as your body’s thermostat, constantly comparing your actual core temperature to a target set point. Under normal conditions, that set point hovers around 98.6°F. During an infection, immune cells detect the invader and release signaling molecules called cytokines. Two of the most important are interleukin-1 and TNF-alpha, both produced by immune cells like macrophages and monocytes. These cytokines travel to the hypothalamus and trigger a chain of chemical reactions that ultimately produces a molecule called prostaglandin E2.

Prostaglandin E2 is the key messenger that actually shifts the set point upward. It acts directly on nerve cells in the preoptic area of the hypothalamus, essentially telling your thermostat that the target should now be 101°F or 102°F instead of 98.6°F. This is why fever-reducing medications work the way they do: they block the enzyme that produces prostaglandin E2, which lets the set point drift back to normal.

What Triggers the Whole Process

The chain of events starts with substances called pyrogens, meaning “fire-starters.” Pyrogens come in two types. Exogenous pyrogens originate outside your body: bacteria, viruses, and their toxins. The most potent is lipopolysaccharide, a component of the outer membrane of certain bacteria like E. coli and Salmonella. Endogenous pyrogens are the signaling molecules your own immune cells produce in response, particularly interleukin-1, TNF-alpha, and other cytokines.

The process typically kicks in within about two hours of exposure to an infectious agent. Immune cells encounter the invader, recognize it as foreign, and begin pumping out cytokines. Those cytokines reach the hypothalamus through the bloodstream, prostaglandin E2 is produced, and the set point rises. Infection is the most common trigger, but inflammation, autoimmune conditions, certain medications, and even some cancers can set off the same cascade.

How Your Body Actually Heats Up

Once the hypothalamus raises its set point, your body has a gap to close. If the new target is 102°F and your current temperature is 98.6°F, your brain perceives a 3.4-degree deficit and responds aggressively. Two main strategies work in parallel.

First, blood vessels near your skin constrict. This diverts warm blood away from the surface and into your core, reducing heat loss through the skin. It’s the same reason your hands and feet get cold in winter. During fever, this vasoconstriction makes your skin feel cool and pale even though your internal temperature is climbing.

Second, your muscles begin to shiver. Shivering is an involuntary, rapid series of muscle contractions that generates heat through the inefficiency of energy use in muscle cells. Research in the Journal of Physiology has shown that when prostaglandin E2 acts on the hypothalamus, it can trigger dramatic increases in muscle activity, along with rises in heart rate and blood pressure, all aimed at driving core temperature up to the new set point. Your body also activates a process called non-shivering thermogenesis, where specialized fat tissue generates heat without muscle contractions.

This is why the onset of a fever feels so counterintuitive. You’re getting hotter inside, but you feel freezing cold and reach for blankets. Your brain is telling you you’re “too cold” relative to the new, higher target.

The Three Phases of a Fever

A fever moves through distinct stages, each with recognizable symptoms. The first is the chill phase, when the set point has just been raised and your body is working to close the gap. You shiver, your skin is pale, and you feel cold. Your heart rate and breathing speed up as your metabolism increases to generate heat.

The second is the flush phase, which begins once your core temperature reaches the new set point. Shivering stops. Blood vessels in the skin dilate again, making your skin warm and flushed. You feel hot, and your temperature plateaus at its elevated level.

The third is defervescence, when the set point drops back to normal, either because your immune system is winning the fight or because you’ve taken a fever-reducing medication. Now your body needs to shed excess heat. Blood rushes to the skin, and you begin to sweat heavily. This is the “breaking” of a fever.

Why Fever Helps Fight Infection

Fever isn’t a malfunction. It’s an evolutionarily conserved response that appears across vertebrate species, which suggests it provides a real survival advantage. Research published in the journal Immunity demonstrated one specific mechanism: at fever-range temperatures (100.4°F to 104°F), T cells become significantly better at reaching sites of infection. The elevated temperature activates a heat-sensitive protein on T cells that helps them stick to blood vessel walls and migrate into infected tissues. In mouse experiments using Salmonella infection, blocking this temperature-sensitive pathway impaired the clearance of bacteria.

Higher temperatures also make blood vessel walls stickier for immune cells in general, increasing the expression of adhesion molecules that help white blood cells latch on and move to where they’re needed. At the same time, many bacteria and viruses reproduce more slowly at temperatures above 98.6°F. So fever works on both sides of the equation: boosting your immune response while slowing the invader.

When Fever Becomes Dangerous

The benefits of fever have limits. Harvard Health defines fever severity in three tiers: low-grade (99.1 to 100.4°F), moderate (100.6 to 102.2°F), and high-grade (102.4 to 105.8°F). Most fevers from common infections stay in the low-to-moderate range and resolve on their own.

Problems emerge above about 104°F (40°C). At this threshold, blood flow to the gut decreases, cell membranes become damaged, and proteins begin to lose their structure, a process called denaturation. Direct cell death in humans begins around 106°F (41°C), and the rate of damage climbs steeply with even small further increases. At these extreme temperatures, the harm from heat itself outweighs any immune benefit. Temperatures this high are rare in typical infections and more commonly result from heat stroke, drug reactions, or severe sepsis rather than the regulated fever process described above.

The distinction matters: a regulated fever is your body intentionally raising the thermostat through the prostaglandin pathway, and it rarely exceeds 104°F on its own. Unregulated hyperthermia, where heat overwhelms the body’s cooling systems, is a different and more dangerous situation because the hypothalamic set point hasn’t changed, yet temperature keeps climbing anyway.