![](https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEgXnl0Wf8fLGqTYTi_meDPIF7jUV4uwVKbcjHakE_jnAiD7EioYuYL7jZ4wvy_zQZ_G4r2H_aixoWCiMdu819VEy02pShaQzoDLGqWq5udrtcyy0RnOvboRO6K7av7lOZVFBVHCTCnBnCpe/s320/2008_polar_ice_min.png)
The most dramatic melting has been seen the last five years, bringing us to a tipping point, that we may have already tipped, that will cause the ice to melt at an exponentially rapid pace.
From the NASA website:
Climate feedbacks are processes that change as a result of a change in forcing, and cause additional climate change. An example of this is the "ice-albedo feedback." As the atmosphere warms, sea ice will melt. Ice is highly reflective, while the underlying ocean surface is far less reflective. The darker ocean will absorb more heat, getting warmer and making the Earth warmer overall. A feedback that increases an initial warming is called a "positive feedback." A feedback that reduces an initial warming is a "negative feedback." The ice-albedo feedback is a very strong positive feedback that has been included in climate models since the 1970s.
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