Climate Oscillations 12: The Causes & Significance

By Andy May

In this post we will examine the idea that ocean and atmospheric oscillations are random internal variability, except for volcanic eruptions and human emissions, at climatic time scales. This is a claim made by the IPCC when they renamed the Atlantic Multidecadal Oscillation (AMO) to the Atlantic Multidecadal Variability (AMV) and the PDO to PDV, and so on. AR6 (IPCC, 2021) explicitly states that the AMO (or AMV) and PDO (or PDV) are “unpredictable on time scales longer than a few years” (IPCC, 2021, p. 197). Their main reason for stating this and concluding that these oscillations are not influenced by external “forcings,” other than a small influence from humans and volcanic eruptions, is that they cannot model these oscillations, with the possible exceptions of the NAM and SAM (IPCC, 2021, pp. 113-115). This is, of course, a circular argument since the IPCC models have never been validated by predicting future climate accurately, and they also make some fundamental assumptions that simply aren’t true.

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Climate Oscillations 11: Oceanic Niño Index (ONI)

By Andy May

The Oceanic Niño Index or ONI is NOAA’s primarily indicator for monitoring the sea surface temperature (SST) anomaly in the critical Niño 3.4 region. It is a 3-month running mean of ERSST.v5 SST anomalies in the Niño 3.4 region, defined as 5°N-5°S and 120°W-170°W. Figure 1 shows the ONI as computed from the NOAA ERSST dataset. ERSST is a two-degree gridded dataset, so the region averaged for figure 1 is 6°N-6°S and 120°W-170°W.

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Climate Oscillations 10: Aleutian Low – Beaufort Sea Anticyclone (ALBSA)

By Andy May

The Aleutian Low – Beaufort Sea Anticyclone climate index or ALBSA is designed to compare the Aleutian Low Pressure and the Beaufort Sea High Pressure Centers. The intent is to relate air circulation patterns in the North Pacific and Arctic to climate and the timing of spring sea ice and snow melt.

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Climate Oscillations 9: Arctic & North Atlantic Oscillations

By Andy May

The Arctic Oscillation (AO) is closely related to the NAO (the North Atlantic Oscillation discussed below) but they are not the same. The NAO is usually measured using the SLP (sea level air pressure) difference between the Azores or the Iberian Peninsula and Iceland and is a North Atlantic regional phenomenon, whereas the Arctic Oscillation is the SLP difference between the northern mid-latitudes and the Arctic, and is evident in all longitudes (Thompson & Wallace, 2001). The AO accounts for more of the variance in Northern Hemisphere surface air temperature than the NAO and is tightly connected to the stratospheric polar vortex (Higgins, et al., 2000) and (Thompson & Wallace, 1998). We will discuss these oscillations together in this post.

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Climate Oscillations 8: The NPI and PDO

By Andy May

The North Pacific Index (NPI) and the Pacific Decadal Oscillation (PDO)

The North Pacific Index (NPI) is computed from the area-weighted sea level air pressure (SLP) over the region 30°N-65°N and 160°E-140°W. It measures interannual to multidecadal variations in Pacific atmospheric circulation. As explained in Trenberth and Hurrel, the winter Aleutian low pressure system moves on a decadal time scale and changes the climate and sea surface temperature (SST) along western North America and in the Northern Central Pacific. These changes are closely related to the PDO (Pacific Decadal Oscillation), which describes the same multidecadal weather and SST pattern in the same region but is calculated with SSTs using a different statistical method. Other oscillations that describe this pattern or something similar are the Interdecadal Pacific Oscillation (IPO) and the North Pacific Oscillation (NPO).

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Review of Politics and Climate Change

By Andy May

I published Politics & Climate Change: A History in 2020, but it has seen a welcome uptick in sales and interest lately. Of note Dr. Patrice Poyet has written a new and updated detailed review of the book that is available on Researchgate here.

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Climate Oscillations 7: The Pacific Mean SST

By Andy May

I originally planned to discuss the North Pacific Index (NPI) in this post, but while researching it, I discovered something interesting about Pacific sea surface temperature (SST) and how it relates to the HadCRUT5 global average surface temperature. As a result, this post is about the total Pacific mean SST and its correlation to HadCRUT5.

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Climate Oscillations 6: Atlantic Meridional Mode (AMM)

By Andy May

The Atlantic Meridional Mode Index (AMM) describes meridional variability in the tropical Atlantic. The area of interest is the ocean area inside 32°N to 21°S and from 75°W to the West African coastline (~15°E). Sometimes the boundaries are given as: 22°S-32°N and 74°W to the West African coast. This is the region where the Intertropical Convergence Zone (ITCZ) exists as it moves north and south with the seasons (Chiang & Vimont, 2004).

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Climate Oscillations 5: SAM

By Andy May

The Antarctic Oscillation (AAO) is also called the Southern Annular Mode or SAM. It is defined as the difference between the zonal (meaning east-west or circumpolar) sea level air pressure between 40°S and 65°S. That is the sea level pressure at 65°S is subtracted from the sea level pressure at 40°S (Gong & Wang, 1999). As the difference increases and SAM becomes more positive, the Southern Hemisphere circumpolar westerly (clockwise as viewed from above the South Pole) winds move closer to Antarctica and generally increase in intensity.

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Climate Oscillations 4: The Length of Day (LOD)

By Andy May

In post 1, I ranked fourteen climate oscillations in Table 1 by their regression statistics against the HadCRUT5 global surface mean temperature. In this regression study the AMO is number one, the Western Hemisphere Warm Pool Area is #2, and the Northern Hemisphere sea ice area is #3. The fourth in importance is the Length of Day or “LOD.” Longer periods (>10 years) of acceleration in Earth’s rotation speed (shorter LOD) correspond to years of increasing zonal (east-west) circulation and global warming, whereas periods of deceleration (longer LOD) indicate less zonal acceleration and periods of cooling (Lambeck & Cazenave, 1976).

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