Liquidity. It’s one of the most frequently used words in finance. It gets invoked to explain virtually everything and anything. But it’s often clear that those invoking it are just parroting things they learned somewhere along the way and don’t truly grasp the mechanics of it. Most don’t even make the basic distinctions among its various forms.
Here’s a rough TL;DR of what you need to know:
There are three basic types of liquidity: Systemic, Credit, and Transactional.
Systemic liquidity can be loosely thought of as the unencumbered resources in the banking system that can be used to settle intra-bank payments. Think Fed funds. And if Fed funds breaks down, payroll doesn’t get made and ATMs run dry. This is what we were on the cusp of in 2008.
But, importantly, Fed funds is a closed system. A bank can draw on its reserves to meet payments to other banks in the system, or, when necessary, get physical cash, but it can’t ‘lend them out’ to clients. Nor can it flood the equity or currency markets with them–contrary to the popular trope. They are not fungible in that way. Only the Federal Reserve can add or withdrawal from the system (with that small exception of physical cash). So, while the composition of reserves across banks can change, the aggregate level in the system cannot unless the Fed wants it to. This type of liquidity is exogenous; it’s all about the Fed.
Credit liquidity is the ability of borrowers to access credit–either to increase debt or roll over existing liabilities. Bank loans, bond issuance, trade finance, whatever. Credit availability is a function of risk appetite, not bank reserves.
It is really hard to disabuse people of the belief in the loanable funds model of credit availability we were all taught in school. This will surprise a lot of people, but the level of Fed fund reserves and credit extension are–even over the long run–uncorrelated.
Don’t believe me? Consider this:
From 1981 to 2006 total credit assets held by US financial institutions grew by $32.3 trillion (744%). How much do you think bank reserves at the Federal Reserve grew by over that same period? They fell by $6.5 billion.
In short, its capitalization ratios and leverage ratios and risk appetite that constrain lending, not reserves.
Think about it this way: If I give my brother an IOU for $100, and he accepts it, we have created credit out of thin air. No cash needed, no reserves liquidated, no assets pledged. He can then sell it to my sister, if he so decides and she trusts my creditworthiness. She then has the claim on me, and we have just created money. If my reputation in her town is sufficiently creditworthy, she could then sell the claim to others, and so forth and so on. No one has to even think about systemic liquidity or the Federal Reserve’s balance sheet, much less be constrained by it. It all comes down to risk appetite, in this case specifically others’ perception of my creditworthiness and their perceived vulnerability should I not make good on it. This is what is called endogenous credit creation.
Transactional, or market-making liquidity is the ease with which market participants can buy and sell financial assets. This is often proxied by bid-ask spreads, volatilities, and market depth. Old hands know how pro-cyclical this type of liquidity is. It is driven by risk appetite, regulatory environment and market structure. This is where things like the Volcker Rule bite. It has virtually nothing to do with the size of the Fed’s balance sheet, either.
The bottom line: Only one of the three fundamental types of liquidity are directly in the hands of the Fed. The other two are pretty much entirely up to our risk appetite. So, next time when someone comes on TV conflating different types of liquidity, you’ll know what time it is.
Source
wonkmonk's notes 