Chapter 2
World Trade: An Overview
◼ Chapter Organization
Who Trades with Whom?
Size Matters: The Gravity Model
Using the Gravity Model: Looking for Anomalies
Impediments to Trade: Distance, Barriers, and Borders
The Changing Pattern of World Trade
Has the World Gotten Smaller?
What Do We Trade?
Service Offshoring
Do Old Rules Still Apply?
Summary
◼ Chapter Overview
Before entering into a series of theoretical models that explain why countries trade across borders and the
benefits of this trade (Chapters 3–11), Chapter 2 considers the pattern of world trade that we observe today.
The core idea of the chapter is the empirical model known as the gravity model. The gravity model is based
on the observations that (1) countries tend to trade with nearby economies and (2) trade is proportional to
country size. The model is called the gravity model, as it is similar in form to the physics equation that
describes the pull of one body on another as proportional to their size and distance.
The basic form of the gravity equation is Tij = A Yi Yj/Dij. The logic supporting this equation is that large
countries have large incomes to spend on imports and produce a large quantity of goods to sell as exports.
This means that the larger that either trade partner is, the larger the volume of trade between them. At the
same time, the distance between two trade partners can substitute for the transport costs that they face as
well as proxy for more intangible aspects of a trading relationship such as the ease of contact for firms. This
model can be used to estimate the predicted trade between two countries and look for anomalies in trade
patterns. The text shows an example where the gravity model can be used to demonstrate the importance
of national borders in determining trade flows. According to many estimates, the border between the
United States and Canada has the impact on trade equivalent to roughly 1,500–2,500 miles of distance.
Other factors such as tariffs, trade agreements, and common language can all affect trade and can be
incorporated into the gravity model.